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Draft plan update, October 10, 2025

Metropolitan Area Planning Council · from the Metropolitan Area Planning Council · 194 pages · 12.2 MB
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TOWN OF WINTHROP 
HAZARD MITIGATION PLAN 
DRAFT 2025 UPDATE 
Draft For Review 
October 10, 2025 
Prepared by 
Metropolitan Area Planning Council 
For the Town of Winthrop

TOWN OF WINTHROP HAZARD MITIGATION PLAN
DRAFT 2025 UPDATE 
ACKNOWLEDGEMENTS AND CREDITS 
This plan was prepared for the Town of Winthrop by the Metropolitan Area Planning Council
(MAPC) under the direction of the Massachusetts Emergency Management Agency (MEMA). The 
plan was funded by the Federal Emergency Management Agency’s (FEMA) Hazard Mitigation 
Grant Program (HMGP). 
MAPC Officers 
President, Erin Wortman, Town of Stoneham 
Vice President, Jennifer Constable, Town of Rockland 
Secretary, Imaikalani Aiu, Town of Weston 
Treasurer, Sam Seidel, Gubernatorial 
Executive Director, Marc Draisen, MAPC 
MAPC Staff Credits 
Project Manager/
Environment Director: Martin Pillsbury 
Mapping/GIS Data Services: Rachel Bower 
Massachusetts Emergency Management Agency 
Agency Director: Dawn Brantley 
Department of Conservation and Recreation 
Commissioner: Brian Arrigo 
Winthrop Hazard Mitigation Planning Team 
Name Position 
Anthony Marino Town Manager 
Cheryl McCormick Assistant Town Manager 
John Goodwin Police Chief 
Scott Wiley Fire Chief 
Steven Calla Director of Public Works Department 
Stephen Calandra Deputy Fire Chief 
Al Legee Building Commissioner 
Chris Boyce Planning Board Chair 
D. Baird Board of Appels Chair 
Kim Dimes Conservation Commission Chair 
Barbara Evangelista Planning Board/Board of Appeals Clerk 
Laurisa Wojcik Executive Assistant to Town Manager 
Steve Rogers Police Dept. 
Ferruccio Romeo Deputy Chief of Policed 
Meredith Hurley Director, Winthrop Public Health and Clinical Services 
Homeyer, Kristen Resilience Manager, N. Suffolk Resilience & Sustainability 
Abderezak Azib Resilience Manager, N. Suffolk Resilience & Sustainability 
Cover photo: Aerial view of Winthrop, Town of Winthrop Linked In page

TOWN OF WINTHROP HAZARD MITIGATION PLAN
DRAFT 2025 UPDATE 
TABLE OF CONTENTS 
Section # Section Page 
1 Executive Summary 1 
2 Introduction 7 
3 Planning Process and Public Participation 16 
4 Risk Assessment 22 
5 Hazard Mitigation Goals 106 
6 Existing Mitigation Measures 107 
7 Mitigation Measures from the 2019 Plan 130 
8 Hazard Mitigation Strategy 139 
9 Plan Adoption and Maintenance 155 
10 List of References 157 
Appendix A Hazard Mapping 158 
Appendix B Hazard Mitigation Team Meetings 174 
Appendix C Documentation of Public Participation 178 
Appendix D Flood Resilience Checklist for Residential Properties 182 
Appendix E Documentation of Plan Adoption 188

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LIST OF TABLES 
Table
# 
Table Page 
1 Plan Review and Update Process 4 
2 Previous Federal/State Disaster Declarations 7 
3 State Disaster Declarations since 2018 10 
4 FEMA-Funded Mitigation Projects 10 
5 Town of Winthrop Characteristics 13 
6 Membership of the Winthrop Hazard Mitigation Team 18 
7 Outreach to Winthrop Community Stakeholders 19 
8 Climate Change & Natural Hazards 29 
9 Hazard Risks Summary 31 
10 Suffolk County Flood Events, 2005-2025 34 
11 Rainfall rates for the 10-year 24-hour storm 36 
12 Suffolk County Coastal Flood Events, 2006-2023 37 
13 Coastal Transect Parameters for Winthrop 38 
14 High Water Marks in Winthrop, Blizzard of 1978 39 
15 Summary of Repetitive Losses and Claims in Winthrop 45 
16 Average Shoreline Change and Uncertainty 47 
17 Average Shoreline change by shoreline type 48 
18 Hurricane Records for Massachusetts, 1938-2023 55 
19 Enhanced Fujita Scale 57 
20 Tornado Records for Suffolk County 59 
21 Dolan- Davis Classification System for Nor’easters 60 
22 Nor ’ easter Events for Massachusetts, 1978 - 2023 61 
23 Regional Snowfall Index 62 
24 Heavy Snow and Blizzard Events in Suffolk County 2010 – 2023 62 
25 Winter-Related Federal Disaster Declarations, 1978-2023 64 
26 Sperry-Piltz Ice Accumulation Index (SPIA®) 66 
27 Beaufort Wind Scale 67 
28 Suffolk County Thunderstorm Events, 2010-2023 70 
29 Hail Size Comparison 71 
30 Suffolk County Hail Events, 2010-2025 72 
31 Richter Scale and Effects 75 
32 Historical Earthquakes in Massachusetts, 1727-2023 76 
33 Landslide Volume and Velocity 79 
34 Suffolk County Extreme Heat Occurrences, 2010-2023 82 
35 Suffolk County Extreme Cold Occurrences, 2010-2023 86 
36 US Drought Monitor Compared to MA Statewide Drought Levels 88 
37 Indices Values Corresponding to Drought Index Severity Levels 89 
38 Chronology of major droughts in Massachusetts since 1879 91 
39 Frequency of Massachusetts Drought Levels 93 
40 Winthrop Land Use 95 
41 Winthrop Employment by Category, 2023 96

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42 Developments Completed Since 2015 98 
43 Winthrop Critical Facilities 99 
44 Estimated Damages from Hurricanes 103 
45 Estimated Damages from Earthquakes 104 
46 Estimated Damages from Flooding 105 
47 Existing Mitigation Measures 124 
48 Status of Mitigation Measures from the 2019 Plan 133 
49 Mitigation Measure Prioritization 146 
50 Recommended Mitigation Measures 150 
LIST OF FIGURES 
Figure
# 
Figure Page 
1 Natural Hazards and Climate Change Overlap 7 
2 Local Retail and Commercial Areas of Winthrop 11 
3 Belle Isle Bridge and Winthrop Ferry 12 
4 Six-Step Planning Process 15 
5 Observed Increase in Temperature 22 
6 Change in the Annual Number of Days Over 90 F 22 
7 Change in Average Summertime Temperatures for Massachusetts 23 
8 Observed Change in Annual Precipitation in the Heaviest 1% Events 24 
9 Change in 2070Annual and Seasonal Precipitation Compared to Today 25 
10 Consecutive dry day events (multiple-dry-day events per year) 26 
11 Observed Increase in Sea Level Rise 27 
12 Total Flooded Area of the Commonwealth for Selected Events 28 
13 Saugus River Gage Heights, March-April 2010 33 
14 Changes in Frequency of Extreme Downpours, 1948 – 2011 34 
15 Suffolk County Shoreline Transect Locations for Winthrop 39 
16 Projected Sea Level Rise for Greater Boston Harbor 41 
17 Areas Inundated in Future Sea Level Rise Scenarios 42 
18 Percent of Assessed Shoreline by Type 47 
19A Long-Term Coastal Erosion in Winthrop, 1840s-2018 49 
19B Short-Term Coastal Erosion in Winthrop, 1970-2019 50 
20 Winthrop Shoreline Change (1847-2008) 51 
21 Atlantic Based Tsunami- Potential Threat 52 
22 Winthrop Shore Drive, October 28, 2012, Hurricane Sandy 56 
23 Chelsea/Revere Tornado of 2014 58 
24 Nor’easter Satellite Image 60 
25 National Risk Index for Lightning 69 
26 Depth-Duration Curve 69 
27 Wildfire Risk Areas in Massachusetts 74 
28 Massachusetts Earthquake Probability Map 77 
29 Boston Study Region Liquefaction Potential 78 
30 Heat Index Chart 81 
31 Health Risks Associated with Extreme Heat 82 
32 Summer 2021 Temperatures, Boston Area 83

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33 Summer 2021 Temperatures, Boston Area 84 
34 Massachusetts Extreme Heat Scenarios 85 
35 Wind Chill Temperature Index and Frostbite Risk 86 
36 Principal Sources and Pattern of Moisture Delivery to Massachusetts 87 
37 Weeks of Extreme Drought (2001-2022) 90 
38 Weeks of Extreme Drought Mapped by MA Region (2001-2017) 92 
39 Recent Massachusetts Drought Events (2016-2021) 92 
40 Winthrop Employment by Category, 2023 96 
41 Winthrop Center Business District 97 
42 Climate Change Effect on Winthrop Residents 114 
43 Climate Action Plan Goals and Objectives 114 
44A Managed Retreat 115 
44B Beach Nourishment 115 
44C Hardscape Seawall/Revetment 116 
44D Nature Based Solution - Cobble 116 
44E Nature Based Solution – Stormwater Parks 116 
44F Nature Based Solution -Oyster Reefs 117 
45 Morton and Banks Streets Hot Spot 117 
46 Priority Sites Assessed 119 
47 Morton and Banks Streets Flood Projections 120 
48 Examples of Neighborhood Flooding, 2018 Nor’easter 121 
49 Winthrop Shoreline Structures 122 
50 Winthrop CRB Top Recommendations 123

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SECTION 1: EXECUTIVE SUMMARY 
Hazard Mitigation planning is a proactive effort to identify actions that can be taken to reduce
the dangers to life and property from natural hazard events. In the communities of the Boston
region of Massachusetts, hazard mitigation planning tends to focus most on flooding, the most
likely natural hazard to impact these communities. Other common concerns are the impacts of 
extreme heat, drought, and nor’easters. This plan also considers how our changing climate will 
affect natural hazards. Warming temperatures will fuel changing precipitation patterns and an
increasing frequency and intensity of severe storms. The Federal Disaster Mitigation Act of 2000
requires all municipalities that wish to be eligible to receive FEMA funding for hazard mitigation
grants to adopt a local multi-hazard mitigation plan and update this plan in five-year intervals. 
PLANNING PROCESS 
Hazard Mitigation planning is a proactive effort to identify actions that can be taken to reduce
the dangers to life and property from natural hazard events. In the communities of the Boston
region of Massachusetts, hazard mitigation planning tends to focus most on flooding, the most
likely natural hazard to impact these communities. However, the plan focuses on all categories of
natural hazards that could potentially affect the community, including those that infrequently
occur. 
The Federal Disaster Mitigation Act of 2000 requires all municipalities that wish to be eligible to
receive FEMA funding for hazard mitigation grants, such as Flood Mitigation Assistance (FMA) and
the Hazard Mitigation Grant Program (HMGP), to adopt a local multi-hazard mitigation plan and
update this plan in five-year intervals. 
This is an update of the 2015 Winthrop Hazard Mitigation Plan, which was approved by FEMA
on August 3, 2015. That plan updated the Town’s original Hazard Mitigation Plan, which
prepared in 2005 as part of a regional North Shore planning effort. 
Planning for this Hazard Mitigation Plan update was led by the Winthrop Local Hazard
Mitigation Team, composed of staff from a number of different Town Departments and
representatives of the North Suffolk Office of Resilience and Sustainability. This team met on the
following dates focusing on various aspects of developing the updated plan: 
July 16, 2024 Identify and map Critical Facilities, Local Hazard Areas, and Development 
October 28, 2024 Review/update Existing Mitigation Measures and Hazard Mitigation Goals 
March 26, 2025 Review the status of recommended mitigation measures from the 2015 plan 
April 15, 2025 Review and finalize the mitigation strategy for the 2025 updated plan 
Public participation in this planning process is important for improving awareness of the potential
impacts of natural hazards and to build support for the actions the Town takes to mitigate them.
The Winthrop Town Council hosted two public meetings, the first on May 20, 2025, and the
second on October xx, 2025. The Town Council meetings were televised locally and available on
videos on You Tube. The meetings included a description of the hazard mitigation planning
process, an overview of the plan and proposed mitigation actions, as well as directions on how

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the public could access the draft plan on the Town website and make comments. The plan was
posted online for public review, and a dedicated project email, WinthropResilience@mapc.org , 
was set up to receive public comments and questions. 
Key town stakeholders and neighboring communities were notified and invited to review the draft
plan and submit comments. See Documentation of Public Meetings in Appendix C. 
RISK ASSESSMENT 
The Winthrop Hazard Mitigation Plan assesses the potential impacts to the Town from flooding,
high winds, winter storms, brush fire, geologic hazards, extreme temperatures, and drought.
Coastal flooding, driven by hurricanes, northeasters and other storms, clearly presents the
greatest hazard to the Town. These are described in Section 4 and the locations of hazard areas
are shown on the map series in Appendix A. The plan also addresses the projected future 
flooding impacts related to sea level rise using the state’s M assachusetts Coastal Flook Risk Model
(MC-FRM). 
The Winthrop Hazard Mitigation Team identified 97 Critical Facilities, four more than in the 2015
plan. These are shown on the map series in Appendix A and listed in Table 43, identifying which
facilities are located within the mapped hazard zones. 
A HAZUS-MH analysis provided estimates of damages from Hurricanes of 100-year and 500-
year recurrence ($6.7 million to $28.1 million) as well as earthquakes of magnitudes 5 and 7 
($375 million to $2.1 billion). Flood damage estimates range from $236 million for a 100-year 
event to $334 million for a 500-year event. 
HAZARD MITIGATION GOALS 
The Winthrop Hazard Mitigation Team reviewed and discussed the goals from the previous 2015
Hazard Mitigation Plan. The Team retained the nine goals from the previous plan for the 2025
update, and endorsed the addition of five new goals (#10 – 15 below) to reflect a more
comprehensive approach and to incorporate climate resiliency for this 2025 plan update. All of
the goals are considered critical for the Town, and they are not listed in order of importance. 
1. Ensure that critical infrastructure sites are protected from natural hazards. 
2. Protect existing residential and business areas from flooding. 
3. Maintain existing mitigation infrastructure in good condition. 
4. Continue to enforce existing zoning and building regulations. 
5. Educate the public about zoning and building regulations, particularly with regard to
changes in regulations that may affect tear-downs and new construction. 
6. Encourage future development in areas that are not prone to natural hazards.

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7. Educate the public about natural hazards and mitigation measures. 
8. Make efficient use of public funds for hazard mitigation. 
9. Protect the Town’s ability to respond to various natural hazard events. 
10. Consider the potential impacts of climate change and incorporate climate
sustainability and resiliency into hazard mitigation planning. 
11. Incorporate environmental justice considerations into natural hazard mitigation,
including outreach to climate vulnerable populations, identification of hazard
impacts, and related mitigation measures. 
12. Integrate hazard mitigation planning as an integral factor in all relevant municipal
departments, committees and boards. 
13. Encourage the business community, local institutions and non-profits to work with
the Town to develop, review and implement the hazard mitigation plan. 
14.: Work with surrounding communities, state, regional and federal agencies to
ensure regional cooperation and solutions for hazards affecting multiple
communities. 
HAZARD MITIGATION STRATEGY 
The Winthrop Local Hazard Mitigation Planning Team identified a number of mitigation measures
that would serve to reduce the Town ’s vulnerability to natural hazard events. These are described
in Section 8 and listed in Table 50. A brief summary list of recommended mitigation measures
follows: 
• Yirrell Beach project 
• Complete utility elevation project in flood hazard area 
• Ingleside Park drainage upgrade 
• Lower Nahant Avenue drainage upgrade 
• Upgrade Bayou Street drain line 
• Lewis Lake drainage upgrade 
• Boston Harbor Drainage Outfall Headwalls / Seawalls 
• Consider Community Rating System application 
• Acquire vacant flood prone lands as or if they become available. 
• Ensure electrical utilities are properly maintained 
• Upgrade emergency generators: Town Hall/EOC 
• Integrate mitigation into local planning 
• Increase hazard education and risk awareness 
• Assess vulnerability to severe winds 
• Implement a structural retrofit program for town’s priority at risk buildings

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• Incorporate drought tolerant species into regulations 
• Require permeable driveways to promote infiltration and reduce runoff 
• Incentivize hazard mitigation (Stormwater fee with incentives) 
Overall, the Town’ hazard mitigation strategy recognizes that mitigating hazards for Winthrop
will be an ongoing process as our understanding of natural hazards and the steps that can be
taken to mitigate their damages changes over time. Global climate change and a variety of other
regional and local factors impact the Town ’s vulnerability, and local officials will need to work
together across municipal lines and with state and federal agencies to address these changes. 
This Hazard Mitigation Strategy is intended to provide the Town with a “roadmap” to key actions 
that will improve its resilience to natural hazards. The plan ’s recommendations will be 
incorporated into other municipal plans and policies, such as the Open Space and Recreation
Plan, , the Capital Investment Plan, and Municipal Vulnerability Preparedness 2.0. 
PLAN REVIEW & UPDATE PROCESS 
The process for developing the Winthrop Hazard Mitigation Plan 2025 Update is summarized in
Table 1 below. 
Table 1 Plan Review and Update Process 
Plan Section Reviews and Updates 
3 – Public
Participation 
The Local Hazard Mitigation Team presented the planning process at
two public meetings hosted by the Town Council. The first meeting was
held during plan development, and the second was held when the
draft plan was completed and made available online for public
comment. Outreach efforts to publicize these engagement
opportunities included webpage content, social media, email, flyers,
and press outreach. 
4 – Risk
Assessment 
MAPC gathered the most recently available hazard and land use
data and met with Town staff to identify changes in local hazard
areas and development trends. Town staff reviewed critical
infrastructure with MAPC staff in order to create an up-to-date
inventory and GIS mapping. MAPC also used the most recently
available version of HAZUS to assess potential impacts of flooding,
earthquakes, and hurricanes. 
5 - Goals The Hazard Mitigation Goals were reviewed and endorsed by the
Winthrop Hazard Mitigation Planning Team. The goals were revised
and added to in order to reflect a more comprehensive approach and
to incorporate climate resiliency for this 2025 plan update. 
6 – Existing
Mitigation
Measures 
The list of existing mitigation measures from the 2015 plan was
updated to reflect current mitigation activities in the Town. 
7 & 8 – Hazard
Mitigation
Strategy 
Mitigation measures from the 2015 plan were reviewed and assessed
as to whether they were completed, in-progress, or deferred. The
Winthrop Hazard Mitigation Team determined whether to carry
forward recommended mitigation measures into this 2025 Plan, or

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modify or delete them. The 2025 Plan's mitigation strategy reflects
both new measures and those carried forward from the 2015 plan
that have not yet been completed. The Winthrop Hazard Mitigation
Team prioritized the mitigation measures based on current conditions. 
9 – Plan
Adoption &
Maintenance 
This section of the plan was updated with an on-going plan
implementation review and five-year update process that will assist
the Town in incorporating hazard mitigation issues into other Town
planning and regulatory review processes and better prepare the
Town for the next comprehensive plan update. 
As indicated on Table xx, Winthrop made progress on implementing mitigation measures
identified in the 2015 Hazard Mitigation Plan. Several recommended mitigation measures have
been completed, including 
• Winthrop Shore Drive seawall 
• Floodplain District Management 
• Floodplain mapping updates 
• Plan for storm surge events. 
• Limit development in V-Zones. 
• Adopt coastal A-Zones. 
• Update building permit to add incentives for additional height above BFE 
• Climate change master plan update or action plan 
• Drainage preventive practices: vactor truck 
• Stormwater best practices training 
• Increase wetlands law enforcement practices 
• Digitally map storm drains and outfalls 
• Wetlands and Stormwater Outreach program 
• Update stormwater ordinance 
• Update tree maintenance program 
• Regional Sea Level Rise Action Work Group participation 
• Partner with utility to document hazard areas 
• Retrofit at-risk critical, public building roofs to withstand snow loads 
• Construct snow fences 
• ID populations vulnerable to long term power outage 
• Include wildfire risk and mitigation in comprehensive planning 
• Inspect fire hydrants on a routine basis 
• Require Green Building and parking best practices 
• Purchase new trailer-mounted light tower 
• Purchase two, 5kW trailer-mounted mobile generators 
• Upgrade radio repeater units

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• Assess and map community risk 
• Winthrop obtained high water rescue vehicles 
• Winthrop obtained an inflatable rescue raft 
Several others are in progress or have been partially completed. Progress toward implementing
these mitigation measures will be continued in this 2025 Plan Update. Moving forward into the
next five-year plan implementation period there will be more opportunities to incorporate hazard
mitigation into the Town ’s decision-making processes. The Hazard Mitigation Team, consisting of
the Town Administrator and representatives of Public Works, Police, Fire, the Planning Board,
Conservation Commission, Building Commissioner, Board of Appeals, Public Health, and the North
Suffolk Office of Resilience and Sustainability, will continue a coordinating role under the
direction of the Town Administrator, as described in Section 9, Plan Adoption and Maintenance.

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SECTION 2: INTRODUCTION 
PLANNING REQUIREMENTS UNDER THE FEDERAL DISASTER MITIGATION ACT 
The Federal Disaster Mitigation Act, passed in 2000, requires that after November 1 2004, all
municipalities that wish to continue to be eligible to receive FEMA funding for hazard mitigation
grants, must adopt a local multi-hazard mitigation plan and update this plan in five-year
intervals. This planning requirement does not affect disaster assistance funding. 
Federal hazard mitigation planning, and grant programs are administered by the Federal
Emergency Management Agency (FEMA) in collaboration with the states. These programs are
administered in Massachusetts by the Massachusetts Emergency Management Agency (MEMA) in
partnership with the Department of Conservation and Recreation (DCR). 
The Town of Winthrop contracted with the Metropolitan Area Planning Council (MAPC), to assist
the Town in updating its local Hazard Mitigation Plan, which was approved by FEMA in 2015. The
updated local plan produced under this contract is designed to meet the requirements of the
Disaster Mitigation Act for the Town of Winthrop, addressing local and regional concerns and
hazards that impact the Town. 
WHAT IS A HAZARD MITIGATION PLAN? 
Natural hazard mitigation planning is the process of determining how to systematically reduce or
eliminate the loss of life and property damage resulting from natural hazards such as floods,
earthquakes, and hurricanes. Hazard mitigation means to permanently reduce or alleviate the
losses of life, injuries, and property resulting from natural hazards through long-term strategies.
These long-term strategies include planning, policy changes, programs, projects, and other
activities. 
As more is understood about the impacts of climate change, it is becoming increasingly important
to recognize the relationship between climate change and many of the natural hazards
addressed in hazard mitigation plans. This was addressed in the last two editions of the
Massachusetts State Hazard Mitigation Plan in 2018 and the 2023. Resilient MA Plan. These
plans recognizes that many hazards are being exacerbated by changing climate, and that
adapting to the expected impacts of climate change is a form of hazard mitigation. Therefore,
this plan incorporates consideration of future risks based on projections for increased
temperatures, future sea level rise, and increased frequency and severity of extreme weather
fueled by global climate change effects. 
Accordingly, MAPC has updated the format of this Hazard Mitigation Plan to incorporate climate
considerations. Figure 1 illustrates the relationship between natural hazards and climate change.

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Figure 1. Natural Hazards and Climate Change 
PREVIOUS FEDERAL/STATE DISASTERS 
The Town of Winthrop has experienced 24 natural hazards that triggered federal or state
disaster declarations since 1991. These are listed in Table 2 below. The majority of these events
involved flooding, while eight were due to hurricanes or nor’easters, and seven were due to
severe winter weather. 
Table 2 Previous Federal Disaster Declarations 
DISASTER NAME
(DATE OF EVENT) TYPE OF ASSISTANCE DECLARED AREAS 
Hurricane Bob 
(August 1991) 
FEMA Public Assistance
Project Grants 
Counties of Barnstable, Bristol, Dukes,
Essex, Hampden, Middlesex, Plymouth,
Nantucket, Norfolk, Suffolk 
Hazard Mitigation Grant
Program 
Counties of Barnstable, Bristol, Dukes,
Essex, Hampden, Middlesex, Plymouth,
Nantucket, Norfolk, Suffolk (16 projects) 
No-Name Storm
(October 1991) FEMA Public Assistance
Project Grants 
Counties of Barnstable, Bristol, Dukes,
Essex, Middlesex, Plymouth, Nantucket,
Norfolk

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DISASTER NAME
(DATE OF EVENT) TYPE OF ASSISTANCE DECLARED AREAS 
No-Name Storm
(October 1991) 
(continued) 
FEMA Individual Household
Program 
Counties of Barnstable, Bristol, Dukes,
Essex, Middlesex, Plymouth, Nantucket,
Norfolk 
Hazard Mitigation Grant
Program 
Counties of Barnstable, Bristol, Dukes,
Essex, Middlesex, Plymouth, Nantucket,
Norfolk, Suffolk (10 projects) 
December Blizzard
(December 1992) 
FEMA Public Assistance
Project Grants 
Counties of Barnstable, Dukes, Essex,
Plymouth, Suffolk 
Hazard Mitigation Grant
Program 
Counties of Barnstable, Dukes, Essex,
Plymouth, Suffolk (7 projects) 
March Blizzard
(March 1993) 
FEMA Public Assistance
Project Grants All 14 Counties 
January Blizzard
(January 1996) 
FEMA Public Assistance
Project Grants All 14 Counties 
October Flood
(October 1996) 
FEMA Public Assistance
Project Grants 
Counties of Essex, Middlesex, Norfolk,
Plymouth, Suffolk 
FEMA Individual Household
Program 
Counties of Essex, Middlesex, Norfolk,
Plymouth, Suffolk 
Hazard Mitigation Grant
Program 
Counties of Essex, Middlesex, Norfolk,
Plymouth, Suffolk (36 projects) 
1997 Community Development
Block Grant-HUD 
Counties of Essex, Middlesex, Norfolk,
Plymouth, Suffolk 
June Flood 
(June 1998) 
FEMA Individual Household
Program 
Counties of Bristol, Essex, Middlesex,
Norfolk, Suffolk, Plymouth, Worcester 
Hazard Mitigation Grant
Program 
Counties of Bristol, Essex, Middlesex,
Norfolk, Suffolk, Plymouth, Worcester
(19 projects) 
(1998) Community Development
Block Grant-HUD 
Counties of Bristol, Essex, Middlesex,
Norfolk, Suffolk, Plymouth, Worcester 
March Flood
(March 2001) 
FEMA Individual Household
Program 
Counties of Bristol, Essex, Middlesex,
Norfolk, Suffolk, Plymouth, Worcester 
Hazard Mitigation Grant
Program 
Counties of Bristol, Essex, Middlesex,
Norfolk, Suffolk, Plymouth, Worcester
(16 projects) 
February Snowstorm
(Feb 17-18, 2003) 
FEMA Public Assistance
Project Grants All 14 Counties 
January Blizzard
(January 22, 2005) 
FEMA Public Assistance
Project Grants All 14 Counties

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DISASTER NAME
(DATE OF EVENT) TYPE OF ASSISTANCE DECLARED AREAS 
Hurricane Katrina
(August 29, 2005) 
FEMA Public Assistance
Project Grants All 14 Counties 
May Rainstorm/Flood
(May 12-23, 2006) 
Hazard Mitigation Grant
Program Statewide 
April Nor’easter 
(April 15-27, 2007) 
Hard Mitigation Grant
Program Statewide 
Flooding 
(March, 2010) 
FEMA Public Assistance 
FEMA Individuals and
Households Program 
SBA Loan 
Bristol, Essex, Middlesex, Suffolk,
Norfolk, Plymouth, Worcester 
Hazard Mitigation Grant
Program Statewide 
Hurricane Earl 
(September 2010) 
FEMA Public Assistance
Project Grants 
Barnstable, Bristol, Dukes, Essex,
Middlesex, Nantucket, Norfolk,
Plymouth, Suffolk, and Worcester 
Tropical Storm Irene 
(August 27-28,
2011) 
FEMA Public Assistance Statewide 
Hurricane Sandy 
(October 27-30,
2012) 
FEMA Public Assistance Statewide 
Severe snowstorm
and Flooding
(February 8-09,
2013 
FEMA Public Assistance;
Hazard Mitigation Grant
Program 
Statewide 
Blizzard of 2015 
(January 26-28,
2015) 
FEMA Public Assistance;
Hazard Mitigation Grant
Program 
Statewide 
Severe winter storm
and Snowstorm 
(January 2018) 
Essex, Middlesex, Norfolk, Suffolk,
Worcester 
Severe winter storm
and flooding 
(March 2018) 
Barnstable, Bristol, Essex, Nantucket,
Norfolk, Plymouth 
COVID-19 Pandemic
(January 2020) 
Statewide 
Source: database provided by MEMA 
Since 2018, there have been five Massachusetts State Declared Disasters that affected Winthrop.
Below is a list of them, which includes several winter storms as well as the Covid-19 pandemic.

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Table 3. State Disaster Declarations since 2018 
Disaster Name Date of Event Declared Areas 
Massachusetts Severe Winter
Storm and Flooding 
March 2-3, 2018 Statewide 
Massachusetts Severe Winter
Storm and Snowstorm 
March 13-14, 2018 Statewide 
Massachusetts Covid-19
Pandemic 
January 20, 2020 – 
May 11, 2023 
Statewide 
Massachusetts Severe Winter
Storm and Snowstorm 
January 28-29, 2022 Statewide 
Massachusetts Hurricane Lee September 15-17,
2023 
Statewide 
Source: FEMA Declared Disasters; OpenFEMA Dataset: Disaster Declarations; and FEMA Declared Disasters. 
FEMA FUNDED MITIGATION PROJECTS 
Over the last 20 years the Town of Winthrop has received funding from FEMA for two mitigation
projects under the Hazard Mitigation Grant Program. These projects totaled $214,004, with
$67,597.50 covered by FEMA grants and $5,000 by local funding. The projects are summarized
in Table 4 below. 
Table 4 FEMA-Funded Mitigation Projects 
Project Title Scope of Work Total Cost Federal
Funding 
Local
Funding 
Point Shirley
Storm Surge
Impact
Reduction
Study 
The proposed scope of
work is for a storm
surge impact study
reduction study to
mitigate flooding in the
Point Shirley Area. 
$20,000.00 $14,210.00 $5,000.00 
Flood
mitigation
Utility Retrofit
Project 
Elevation of utilities
above base flood
elevation for 20
properties $194,004.00 $53,387.50 $0.00 
Source: database provided by MEMA

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COMMUNITY PROFILE 
The Town of Winthrop is a municipality in Suffolk County, Massachusetts, United States. The
population of Winthrop was 19,031 at the 2020 U.S. Census. It is an ocean-side suburban
community situated at the north entrance to Boston Harbor and is very close to Logan International
Airport. The Town is a peninsula, 1.6 square miles (4.2 km2) in area, connected to Revere by a
narrow isthmus and to East Boston by a bridge over the harbor inlet to the Belle Isle Marsh
Reservation. Settled in 1630, Winthrop is one of the oldest communities in the United States. It is
also one of the smallest and most densely populated municipalities in Massachusetts. 
Winthrop has a reputation for being a safe and pleasant place to live. Winthrop is a close-knit,
family-oriented community where everything is within walking distance. There is a public bus route
which travels throughout the Town and connects to the Orient Heights stop on the Blue Line of the
MBTA A seasonal ferry provides water transportation to downtown Boston. There are numerous
parks and playgrounds, six public beaches, four tennis courts, five athletic fields, a public landing
for boats and an indoor skating rink. There is a youth center as well as a senior center which both
offer many activities and programs. 
Winthrop Center offers a multitude of shops as well as small clusters of stores in other sections of
the Town. Local retail and commercial areas are shown on Figure 2. There are numerous
physicians and dentists in the community as well as a community ambulance service. Public
facilities include gas, sewer, water, electricity and cable to the entire Town and trash is collected
weekly with provision for recycling. 
Figure 2 Local Retail and Commercial Areas of Winthrop 
Source: Winthrop 2030, MAPC

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Additionally, active organizations include the Chamber of Commerce, Rotary, American Legion,
Amvets, Little League, Soccer Association, Elks, Sons of Italy, Boy and Girl Scouts, Historical
Society, Council on Aging, Winthrop Playmakers, three yacht clubs, and a golf club. 
Transportation and Connectivity 
One of the most important features of Winthrop to consider for any hazard mitigation is the 
town’s location on a peninsula where Boston Harbor meets the Atlantic Ocean. Being surrounded
by coastal waters on three sides, Winthrop has very limited transportation connections to the 
mainland. The Town’s Community Resilience Building report notes that: 
Access to the Town of Winthrop is primarily along Route 145, 
Winthrop Parkway or across the Belle Isle Bridge (Main Street).
Winthrop Parkway connects the town to Revere along a narrow strip of
land and this connection has been closed by the Town of Revere in the
past due to storm conditions resulting in unsafe passage. With only two
main roadways to access Winthrop, managing this infrastructure is
critical for emergency evacuation and response. Or, if evacuation and
response is not possible, managing isolation and sheltering in place 
becomes critical. 
In addition to road access, a passenger ferry connects Winthrop to downtown Boston. However,
during extreme storm events this would not be available to aid in evacuating residents. 
Figure 3 Belle Isle Bridge and Winthrop Ferry 
Resilient Winthrop , Stantec/Woods Hole Group Photo: M. Pillsbury 
Resilient Winthrop also underscores the critical nature of Winthrop’s limited roadway connectivity: 
With only two roadways to access the Winthrop peninsula, the resilience of transportation
infrastructure is particularly important for emergency evacuation and response. Roads play an
important role in disaster recovery efforts by providing access to damaged areas for
emergency responders and construction equipment.

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The Town’s Climate Action Plan also emphasizes the importance of connectivity and evacuation 
routes: “ Flooding occurs on critical path evacuation routes, including Main Street, Shirley Street,
Washington Street and Pleasant Street, creating a public safety issue ” 
Demographic Characteristics 
The 2020 population of Winthrop was 19,031 people and there were 8,242 households.
(2020 US Census, 2017-21 American Community Survey). The significant demographic
characteristics of the Town of Winthrop are summarized in Table 5. Some of these features are
important to keep in mind for hazard mitigation as well as emergency preparedness and
response in the Town. 
Table 5. Town of Winthrop Characteristics 
Population 
Total population 19,031 
Residents under 5 years old 4.4% 
Residents 65 years old and over 20.2% 
Race & Ethnicity 
American Indian and Alaska Native 48 
Asian 293 
African American 790 
White 15,031 
Hispanic or Latino 2,533 
Other Race 894 
Two or More Races 993 
Household Income 
Total Households 8,242 
Median Household Income $86,780 
Renter occupied housing units 41.1% 
Languages 
Speak a language other than English at home 
Spanish 2230 
Other Indo-European languages 2283 
Asian and Pacific Island languages 269 
Other languages 157 
Speaks English less than “very well” 2.6% 
Residents with a Disability 29.8% 
Age 65 and over with a disability 6.3% 
Households in Poverty 12.2% 
Households with no vehicle 12.5% 
Households with no internet service 12.8% 
Sources: US Census, 2020 Decennial Census and American Community Survey (ACS) 
5-Year Estimates (2017-2021)

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Environmental Justice Populations 
There are seven Environmental Justice census block groups in Winthrop designated by the MA
Executive Office of Energy and Environmental Affairs. An environmental justice population is a
neighborhood where one or more of the following criteria are true: 
• Median household income is 65 percent or less of the statewide median household income 
• Minorities make up 40 percent or more of the population 
• 25 percent or more of households identify as speaking English less than "very well" 
In Winthrop, four census block groups are designated Environmental Justice based on minority
population and three are designated based on median household income. None of the block
groups meet the criteria for limited English. See Map 1A in Appendix A. 
Water Resources 
Winthrop is located within the Mystic River Watershed and within the Boston Harbor Subbasin.
The Mystic River Watershed is a densely populated and very urban watershed with a long history
of industrial development and pollution. Water quality issues stem from a variety of sources
including stormwater runoff, point source pollution, contaminated sediments in the river due to
industrial uses, lack of access to open space as well as invasive species. A large number of
community organizations as well as New England EPA and the Mystic River Watershed 
Association are actively working to improve water quality and access to open space. 
There are no rivers or streams within the town. The only body of surface water is Lewis Lake. Belle 
Isle Inlet to the north forms the boundary between Boston and Winthrop. Therefore, the major 
water quality issue in Winthrop is the health of Boston Harbor and its impact on the cleanliness of 
the beaches. 
Lewis Lake receives stormwater runoff from approximately 1/3 of the town. The lake is only a
few inches deep because of siltation from run-off. The upper lake is freshwater and the lower
lake is brackish water and saltwater. The edge of the lake is very weedy with phragmites. There
is a manually operated tidal gate. The lake needs to be dredged or it will eventually fill in and
be unable to hold and absorb stormwater runoff. The town is investigating installing a closed
drainage pipe in the existing culvert and swale along Veterans Road as well as installation of an
automatic tide gate.

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SECTION 3: PLANNING PROCESS & PUBLIC PARTICIPATION 
MAPC employs a planning process based on FEMA’s hazard mitigation planning guidance 
focusing on local needs and priorities, but maintaining a regional perspective matched to the
scale and nature of natural hazard events. Public participation is a central component of this
process, providing critical information about the local occurrence of hazards while also serving as
a means to build a base of support for hazard mitigation activities. 
MAPC supports participation by the general public and other plan stakeholders through: 
• Four meetings and coordination with the Local Hazard Mitigation Team 
• Two public meetings, advertised through email, webpage content, a flyer, press release to
local media, and social media posts, and made available town-wide on Local Access TV, 
• A project website at: www.mapc.org/resource-library/winthrop-hmp and a dedicated 
email for public comments, WinthropResilience@mapc.org 
• Opening a public comment period at the second public meeting, and posting the draft
plan to the project website to facilitate public review, 
• Outreach to neighboring communities, boards and commissions, the local chamber of
commerce and businesses, environmental NGO’s, social service providers, and other local
or regional stakeholders. 
PLANNING PROCESS SUMMARY 
The six-step planning process outlined below and in Figure 4 is based on the guidance provided
by FEMA in the Local Multi-Hazard Mitigation Planning Guidance. The process focuses on local
problem areas and identifies needed mitigation measures based on where gaps occur in the
existing mitigation efforts of the municipality. The planning process allows municipal staff to bring
the most recent hazard information into the plan, including new hazard occurrence data, changes 
to a municipality’s mitigation measur es, and progress made on actions identified in previous plans. 
Figure 4: Six-Step Planning Process

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1. Map the Hazards – MAPC relies on data from a number of different federal, state, and local 
sources in order to map the areas with the potential to experience natural hazards. This
mapping represents a multi-hazard assessment of the municipality and is used as a set of
base maps for the remainder of the planning process. A particularly important source of
information is the knowledge drawn from local municipal staff on where natural hazard
impacts have occurred, which is collected. These maps can be found in Appendix A. 
2. Assess the Risks & Potential Damages – Working with local staff, critical facilities,
infrastructure, vulnerable populations, and other features are mapped and contrasted with the
hazard data from the first step to identify those that might represent particular vulnerabilities
to these hazards. Land use data and development trends are also incorporated into this
analysis. In addition, MAPC develops estimates of the potential impacts of certain hazard
events on the community. MAPC drew on the following resources to complete the plan: 
• Town of Winthrop, General Bylaws 
• Town of Winthrop, Zoning Bylaw 
• Town of Winthrop, Business District Master Plan, 2017 
• Town of Winthrop, Climate Action Plan for Winthrop, 2025 
• Town of Winthrop, Municipal Vulnerability Preparedness, 2018 
• Town of Winthrop, Stormwater Management Program Plan, 2022 
• Town of Winthrop, Open Space and Recreation Plan, 2014 
• Town of Winthrop, Resilient Winthrop, Designing Coastal Infrastructure for Climate
Change 
• Town of Winthrop, Winthrop 2030 
• Blue Hills Observatory 
• Environment America Research and Policy Center, When It Rains It Pours – Global
Warming and the Increase in Extreme Precipitation, July 2012 
• FEMA, Disaster Declarations for States and Counties, 1978-2025 
• FEMA, Flood Insurance Study, Suffolk County, 2024 
• FEMA Flood Insurance Rate Maps for Suffolk County, MA, 2016 
• FEMA, HAZUS-MH, 2023 
• FEMA, Local Mitigation Planning Policy Guide, 2025 
• Massachusetts Climate Change Assessment, 2022 
• Massachusetts Report of the MA Coastal Erosion Commission, 2016 
• MA Office of Coastal Zone Management, Sea Level Rise: Understanding and
Applying Trends and Future Scenarios for Analysis and Planning, December 2013. 
• MA Office of Dam Safety, Inventory of Massachusetts Dams 
• Massachusetts State Hazard Mitigation and Climate Adaptation Plan, 2018, 2023 
• Massachusetts State Hazard Mitigation Plan, 2013 
• Metropolitan Area Planning Council, Winthrop Climate Resilient Land Use Project 
• Metropolitan Area Planning Council, GIS Lab, Regional Plans and Data. 
• New England Seismic Network, Boston College Weston Observatory 
• NOAA Centers for Environmental Information 
• Northeast States Emergency Consortium 
• Tornado History Project

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• US Census, 2020, American Community Survey2017-21 
• USDA Forest Service, Wildfire Risk to Communities 
• USGS, National Water Information System 
• U.S. Global Change Research Program, Fourth National Climate Assessment, 2018 
3. Review Existing Mitigation – Municipalities in the Boston Metropolitan Region have an active
history in hazard mitigation as most have adopted flood plain zoning districts, wetlands
protection programs, and other measures as well as enforcing the State building code, which
has strong provisions related to hazard resistant building requirements. All current municipal
mitigation measures are documented in the plan. 
4. Develop Mitigation Strategies – MAPC works with the local municipal staff to identify new
mitigation measures, utilizing information gathered from the hazard identification, 
vulnerability assessments, and the community’s existing mitigation efforts to dete rmine where
additional work is necessary to reduce the potential damages from hazard events. Additional
information on the development of hazard mitigation strategies can be found in Chapter 7. 
5. Plan Approval & Adoption – Once a final draft of the plan is complete it is sent to MEMA for
the state level review and, following that, to FEMA for approval. Typically, once FEMA has
approved the plan the agency issues a conditional approval (Approval Pending Adoption),
with the condition being adoption of the plan by the municipality. More information on plan
adoption can be found in Chapter IX and documentation of plan adoption can be found in
Appendix E. 
6. Implement & Update the Plan – Implementation is the final and most important part of any
planning process. Hazard Mitigation Plans must also be updated on a five-year basis making
preparation for the next plan update an important on-going activity. Chapter IX includes
more detailed information on plan implementation. 
THE LOCAL HAZARD MITIGATION PLANNING TEAM 
MAPC worked with the municipal leadership to convene and facilitate a local Hazard Mitigation
Planning Team for Winthrop. MAPC briefed the municipality as to the desired composition of that
team as well as the need for outreach to stakeholders such as the business community, civic
organizations and citizens. The team was composed of staff and local officials from a number of
different Town Departments and representatives of the North Suffolk Office of Resilience and
Sustainability. The Winthrop Hazard Mitigation Planning Team membership can be found in Table
6 below. 
The Hazard Mitigation Team is central to the planning process as it is the primary body tasked
with developing a mitigation strategy for the community. The local team was tasked with working
with MAPC to set plan goals, provide information on the hazards that impact the Town, existing
mitigation measures, and help to develop new mitigation measures for this plan update. 
The team met on the following dates focusing on various aspects of developing the updated plan:

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July 16, 2024 Identify and map Critical Facilities, Local Hazard Areas, and Development 
October 28, 2024 Review/update Existing Mitigation Measures and Hazard Mitigation Goals 
March 26, 2025 Review the status of recommended mitigation measures from the 2015 plan 
April 15, 2025 Review and finalize the mitigation strategy for the 2025 updated plan 
Table 6: Membership of the Winthrop Hazard Mitigation Team 
Name Position 
Anthony Marino Town Manager 
Cheryl McCormick Assistant Town Manager 
John Goodwin Police Chief 
Scott Wiley Fire Chief 
Steven Calla Director of Public Works Department 
Stephen Calandra Deputy Fire Chief 
Al Legee Building Commissioner 
Chris Boyce Planning Board Chair 
D. Baird Board of Appeals Chair 
Kim Dimes Conservation Commission Chair 
Barbara Evangelista Planning Board/Board of Appeals Clerk 
Laurisa Wojcik Executive Assistant to Town Manager 
Steve Rogers Police Dept. 
Ferruccio Romeo Deputy Chief of Policed 
Meredith Hurley Director, Winthrop Public Health and Clinical Services 
Homeyer, Kristen Resilience Manager, N. Suffolk Resilience & Sustainability 
Abderezak Azib Resilience Manager, N. Suffolk Resilience & Sustainability 
Under Massachusetts Home Rule law and tradition, the Town of Winthrop has primary
responsibility for regulating development in town. The Winthrop Planning Board and the
Conservation Commission are the primary local agencies responsible for regulating development
in town. The Board of Appeals and the Building Commissioner also have key responsibilities for
development in Winthrop. Their feedback on development of the plan was assured through the
participation of the Chairmen of the Planning Board, Conservation Commission, and Board of
Appeals as well as the Building Commissioner on the local Hazard Mitigation Team.. In addition,
MAPC, as the State designated regional planning agency for Winthrop, works with all agencies
that regulate development and infrastructure in the region, including the l municipal entities and
state agencies, such as MassDOT, the Massachusetts Dept. of Conservation and Recreation and
the Massachusetts Water Resources Authority. 
PUBLIC MEETINGS 
Public participation in the hazard mitigation planning process is important, both for plan
development and for later implementation of the plan. Residents, business owners, and other
community members can be a good source for information on the historical and potential impacts
of natural hazard events and particular vulnerabilities the community may face from these
hazards. Their participation in the planning process also builds understanding of the concept of

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hazard mitigation, potentially creating support for mitigation actions taken in the future to
implement the plan. 
Public participation in this planning process is important for improving awareness of the potential
impacts of natural hazards and to build support for the actions the Town takes to mitigate them. 
The public had an opportunity to provide input to the hazard mitigation planning process at two
public meetings, one during the planning process and one after a complete draft plan is available
for review. The Winthrop Town Council hosted the public meetings, the first on May 20, 2025,
and the second on October xx, 2025. The Town Council meetings were publicized according to
Massachusetts Open Meeting Law and were televised locally and available on videos on You
Tube. Both meetings were publicized on the To wn’s website and social media, and direct outreach 
by email. A Media Advisory was also sent to the local press. 
The first meeting featured an overview of the hazard mitigation planning process, and summary
of the plan and mitigation actions. The draft plan was presented at the second public meeting.
The plan was posted online on the project web page for public access to review and comment on
the plan. and a dedicated project email, WinthropResilience@mapc.org , was set up to receive 
public comments and questions. Key town stakeholders and neighboring communities were notified
and invited to review the draft plan and submit comments. See Documentation of Public Meetings
in Appendix C. 
LOCAL STAKEHOLDER INVOLVEMENT 
The Town reached out to local stakeholders that might have an interest in the Hazard Mitigation
Plan including neighboring communities, agencies, businesses, nonprofits, and other interested
parties. Notice was sent to the following organizations and neighboring municipalities inviting
them to review the Hazard Mitigation Plan and submit comments to the Town: 
Table 7: Winthrop Community Stakeholders 
Cat Pedmonti Mystic River Watershed Association 
Cindy Baxter Friends of Belle Isle Marsh 
John DaRos Winthrop Town Councilor, Precinct 6 
Town of Winthrop Winthrop Climate Commission 
Town of Winthrop Citizens Advisory Committee on Climate 
Town of Winthrop Council on Aging 
City Clerk City of Boston 
City Clerk City of Revere 
The draft plan was posted online for public review, The Town received [TBD] comments, which are
included in Appendix C. 
CONTINUING PUBLIC PARTICIPATION 
Following the adoption of the plan update, the planning team will continue to provide residents,
businesses, and other stakeholders with the opportunity to learn about the hazard mitigation 
planning process and to contribute information that will update the town’s understanding of local

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hazards. As the review of the plan is conducted by the Hazard Mitigation Team, these will be 
placed on the Town’s web site, and any meetings of the Hazard Mitigation Team will be publicly
noticed in accordance with town and state open meeting laws. 
PLANNING TIMELINE 
PLAN UPDATE PROCESS 2024-25 
July 16, 2024 1 st Meeting of the Winthrop Hazard Mitigation Team 
October 28, 2024 2 nd Meeting of the Winthrop Hazard Mitigation Team 
March 26, 2025 3 rd Meeting of the Winthrop Hazard Mitigation Team 
April 15, 2025 4 th Meeting of the Winthrop Hazard Mitigation Team 
May 20, 2025 Public Meeting #1 hosted by the Town Council 
Oct. xx, 2025 Public Meeting #2 hosted by the Town Council 
PLAN IMPLEMENTATION MILESTONES 2026-30 
After this plan update is approved by FEMA for a five-year period, the Town should take note of
the following milestones for the ongoing implementation, review, and updating of this plan: 
2028 Conduct Mid-Term Plan Survey on Progress 
2029 Seek FEMA grant to prepare next plan update 
2030 Begin process to update the plan 
2031 Submit Draft 2031 Plan Update to MEMA and FEMA 
2031 FEMA approval of 2030 Plan Update

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SECTION 4: RISK ASSESSMENT 
The risk assessment analyzes the potential natural hazards that could occur within the Town as
well as the relationship between those hazards and current land uses, potential future
development, and critical infrastructure. This section also includes a vulnerability assessment that
estimates the potential damages that could result from certain large-scale natural hazard events. 
In order to update Marlborough’s risk assessment, MAPC gathered the most recently available 
hazard and land use data and met with the Local Team to identify changes in local hazard areas 
and development trends. MAPC also used FEMA’s damage estimation software, Hazards US 
(HAZUS). 
The projected impacts of our warming climate on natural hazards are integrated throughout this
risk assessment. Key impacts include rising temperatures, which in turn affect precipitation patterns
and extreme weather. Analysis of these impacts included in this plan aligned closely with the data 
and assessment presented in Massachusetts’ State Hazard Mitigation and Climate Adaptation
Plan (SHMCAP) and the Massachusetts’ 2022 Climate Change Assessment. 
CLIMATE CHANGE OBSERVATIONS AND PROJECTIONS 
Climate change observations come from a variety of data sources that have measured and
recorded changes in recent decades and centuries. Climate change projections, however, predict
future climate impacts and, by their nature, cannot be observed or measured. As a result of the
inherent uncertainty in predicting future conditions, climate projections are generally expressed as
a range of possible impacts. 
TEMPERATURE 
Our climate has always been regulated by gases, including carbon dioxide, methane, and nitrous
oxide, which blanket the earth. These gases trap heat that would otherwise be reflected out to
space; without them our planet would be too cold to support life. We refer to these gases as 
“greenhouse gases” (GHGs) for their heat trapping capacity. The combustion of fossil fuels, our 
primary energy source in the age of industrialization, releases GHGs into the atmosphere. In the
past century, human activity associated with industrialization has contributed to a growing
concentration of GHGs in our atmosphere. Records from the Blue Hill Observatory in Milton, MA
show that average temperatures (30-year mean) have risen approximately 3 degrees (F) in the
almost 200 years since record keeping began in 1831. See Figure 5 below for more information. 
“Global climate is changing rapidly compared to the pace of natural variations in climate
that have occurred throughout Earth’s history. Global average temperature has increased 
by about 1.8°F from 1901 to 2016, and observational evidence does not support any
credible natural explanations for this amount of warming; instead, the evidence
consistently points to human activities, especially emissions of greenhouse or heat- 
trapping gases, as the dominant cause.” 
Fourth National Climate Assessment, 2018 (Chapter 2-1)

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Figure 5: Observed Increase in Temperature 
Climate projections include an increase in average temperature and in the number of extreme
heat days. Extreme cold days are projected to decrease in number. By 2030, the summer mean
temperature could increase by 3.6°F from the historical period (1950-2013). By 2070, there
could be 58 fewer days below freezing, which could lead to an increase in ticks. By mid-century,
the State anticipates about 25 more days per year where the temperature exceeds 90°F for
inland areas, and about 19 more days above 90°F for coastal areas (Commonwealth of
Massachusetts, 2022). 
Figure 6: Change in the Annual Number of Days Over 90  F Compared to Today 
Sources: 2022 MA Climate Change Assessment and Stochastic Weather Generator

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These changes could result in Massachusetts summers feeling like a more southern state, as
described in the infographic in Figure 7 from the State’s 2022 Climate Change Assessment. 
Figure 7: Change in Average Summertime Temperatures for Massachusetts 
Source: 2022 MA Climate Change Assessment 
PRECIPITATION PATTERNS 
Annual precipitation in Massachusetts has increased by approximately 10% in the fifty-year
period from 1960 to 2010 (MA EEA, 2011). Moreover, there has been a significant increase in
the frequency and intensity of large rain events. For the Northeast US, according to the Fourth
National Climate Assessment 2018, in the past sixty years there has been a 55% increase in the
amount of annual precipitation that falls in the top 1% of storm events, as shown in Figure 8
below (US Global Change Research Program, 2018). Changes in precipitation are fueled by
warming temperatures which increase evaporation and, therefore, the amount of water vapor in
the air.

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Figure 8: Observed Change in Total Annual Precipitation in the Heaviest 1% Events 
Source: Fourth National Climate Assessment, 2018 
Numbers circled in black indicate % change. 
Massachusetts’ 2022 Climate Change Assessment anticipates that most parts of the State will see 
a future increase in annual total precipitation of less than 8% per year. Most of these increases
are anticipated during the winter months (see Figure 9 below). 
Additionally, t he historic 10% annual chance daily rainfall event (2.8- 4.0” of rain) could occur 
four times more frequently by 2090 (Commonwealth of Massachusetts, 2022).

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Figure 9: Change in Annual and Seasonal Precipitation in 2070 Compared to Today 
Source: 2022 MA Climate Change Assessment. The current climate is the 1986-2005 era, the projection for 2070 is for
a 20-year era centered on 2070. Maps show LOCA downscaled GCM projections at the 50th percentile across 20 LOCA
GCMs that overlap with the GCMs used in the Stochastic Weather Generator. 
Despite overall increasing precipitation, more frequent and significant summer droughts are also
a projected consequence of climate change. This is due to projections that precipitation will
increase in winter and spring and decrease slightly in the summer and, as a result of earlier snow 
melt, and higher temperatures that will reduce soil moisture. Massachusetts’ 2022 Climate Change 
Assessment anticipates that these changes will vary by region. The North and South Shore region
where Winthrop is located may experience slightly more consecutive dry days, and significantly
more days without rain per year, by 2090 (Commonwealth of Massachusetts, 2022). See Figure
10 below for more information.

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Figure 10: Consecutive dry day events (number of multiple-dry-day events per year) 
Source: 2022 MA Climate Change Assessment. The Town of Winthrop is located in the North & South Shores region. 
SEA LEVEL RISE 
High-level information on sea level rise is discussed here as the town as well as the regional
economy of the Boston Metro area may be impacted by sea level rise in the future. Warming
temperatures contribute to sea level rise in three ways. First, warm water expands to take up
more space. Second, rising temperatures are melting land-based ice which enters the oceans as
melt water. A third, quite minor, contributor to sea level rise in New England is not related to
climate change. New England is still experiencing a small amount of land subsidence (drop in
elevation) in response to the last glacial period. NOAA’s records from the Boston Tide Station 
show nearly one foot of sea level rise over the past century. See Figure 11 below for more
information.

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Figure 11: Observed Increase in Sea Level Rise 
Source: NOAA 
The sea level rise information in Massachusetts’ 2022 Climate Change Assessment considers sea -
level changes, land-level changes, and other regional facts that can impact the rate of change.
The report includes the following approximate sea level rise projections for the State: 
• Northern Massachusetts: 21 inches by 2050, and 43 inches by 2070 
• Southern Massachusetts: 23 inches by 2050 and 45 inches by 2070 
The 2022 Climate Change Assessment also quantified the developed land area flooded for
events including: 
• the 20-year (5% annual probability) 
• 100-year (1% probability) 
• 1000-year (0.1% probability) events 
This approach found that the area flooded by the current 1000-year event is comparable to the
area of a 20-year event by 2050. Even more areas could be impacted by the annual probability
event by 2070. See Figure 12 below for more information.

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Figure 12: Total Flooded Area of the Commonwealth for Selected Events 
Source: 2022 MA Climate Change Assessment 
CLIMATE CHANGE AND HAZARD MITIGATION 
Following the outline of the Massachusetts State Hazard Mitigation and Climate Adaptation Plan
(SHMCAP), this local hazard mitigation plan organizes consideration of natural hazards based on
their relationship to projected climate changes. 
Table 8 below, which is originally from the 2018 SHMCAP, summarizes the natural hazards
reviewed in this plan, climate interactions, and expected impacts.

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Table 8: Climate Change & Natural Hazards 
Primary Climate
Change Interaction Natural Hazard Other Climate Change
Interactions 
Representative 
Climate Change Impacts 
Changes in
Precipitation 
Inland Flooding Extreme Weather Flash flooding, urban flooding, drainage
system impacts (natural and human-
made), lack of groundwater recharge,
impacts to drinking water supply, public
health impacts from mold and worsened
indoor air quality, vector-borne diseases
from stagnant water, increased potential
for loss of life, episodic drought, changes
in snow-rain ratios, changes in extent
and duration of snow cover,
degradation of stream channels and
wetland 
Drought 
Rising
Temperatures,
Extreme Weather 
Landslide 
Rising
Temperatures,
Extreme Weather 
Sea Level Rise 
Coastal Flooding Extreme Weather Increase in tidal and coastal floods, storm
surge, coastal erosion, marsh migration,
inundation of coastal and marine
ecosystems, loss of wetlands 
Coastal Erosion Extreme Precipitation 
Tsunami Rising Temperatures 
Rising
Temperatures 
Average/Extreme
Temperatures N/A Shifting in seasons (longer summer, early
spring, including earlier timing of spring
peak flow), increase in length of growing
season, increase of invasive species,
increase in vector-borne illnesses (West
Nile, Zika, EEE), ecosystem stress, energy
brownouts from higher energy demands,
more intense heat waves, public health
impacts from high heat exposure and
poor outdoor air quality, increased
potential for loss of life, drying of
streams and wetlands, eutrophication of
lakes and ponds 
Wildfires Changes in Precipitation 
Invasive Species 
Changes in
Precipitation, Extreme
Weather 
Extreme Weather 
Hurricanes/Tropical
Storms 
Rising Temperatures,
Changes in
Precipitation 
Increase in frequency and intensity of
extreme weather events, resulting in
greater damage to natural resources,
property, and infrastructure, as well as
increased potential for loss of life 
Severe Winter Storm / 
Nor’easter 
Tornadoes 
Other Severe Weather
(Strong Wind &
Thunderstorms)

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31 
UPDATE PROCESS 
In order to update Winthrop ’s risk assessment, MAPC gathered the most recently available 
hazard and land use data from federal and state sources and met with Town ’s Hazard Mitigation 
Team to identify changes in local hazard areas and development trends. The local Team also
reviewed critical infrastructure with MAPC staff in order to create an up-to-date inventory and
accompanying GIS map. MAPC also used the most recently available version of FEMA’s HAZUS-
MH program (described below) to assessed the potential impacts of Hurricanes, Tornadoes, and
Flooding. 
OVERVIEW OF HAZARDS AND IMPACTS 
The risk assessment analyzes the potential natural hazards that could occur within the Town of
Winthrop as well as the relationship between those hazards and current land uses, potential
future development, and critical infrastructure. This updated plan also recognizes that climate
change is projected to have significant impacts on many natural hazards in Winthrop. The
Resilient MA Plan (2023), the Massachusetts Climate Change Assessment (2022), and the
SHMCAP (2018) are key planning documents that examine natural hazards and climate trends
that have the potential to impact the Commonwealth. The 2013 State HMP set the stage by
defining considerations such as frequency and severity and summarizing the frequency and
severity of hazards of greatest concern. The 2018 SHMCAP used similar definitions for hazard
considerations and expanded on this research by including additional climate projections. Because
the 2013 State HMP includes definitions that were not specified in the SHMCAP, both resources
are referred to in this report. 
Table 9 below summarizes the hazard risks for Winthrop, with reference to the hazards in
Massachusetts. This evaluation takes into account the frequency and severity of each hazard for
Massachusetts and Winthrop, based on available data, including: 
• State-level data, including the Resilient MA Plan, the 2022 Climate Change
Assessment, and 2018 SHMCAP. 
• County-level data from NOAA’s National Climatic Data Center and Storm Events 
Database for Suffolk County (where Winthrop is located) 
• Local-level information including input from the Local Team, the hazard mapping
included in Appendix A, and the HAZUS results. 
The statewide hazard risk assessment is based on the definitions for hazard frequency and
severity listed below. The statewide assessment was modified to reflect local conditions in
Winthrop using the same criteria.

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Table 9 - Hazard Risks Summary 
Hazard Frequency Severity 
Massachusetts Winthrop Massachusetts Winthrop 
Flooding from
Precipitation 
Very High High Serious Serious 
Dam failures Very Low N/A Extensive N/A 
Coastal Erosion Very High Very High Serious-Extensive Extensive 
Coastal Flooding Very High Very High Serious-Extensive Extensive 
Tsunami Very Low Very Low Extensive-Catastrophic Extensive-
Catastrophic 
Hurricane/Tropical Storm Medium Medium Serious - Catastrophic Extensive 
Tornadoes High Low Serious - Extensive Serious 
Other Severe Weather
(Thunderstorms/Hail) 
Very High High Minor - Extensive Minor-Serious 
Severe Winter/ 
Nor’easter /Blizzards 
High High Minor - Extensive Extensive 
Winter-Ice Storms Medium Medium Minor - Extensive Minor 
Earthquakes Medium Medium Serious - Catastrophic Serious 
Landslides High Very Low Minor - Extensive Minor 
Wildfire/Brushfires Very High Medium Minor - Extensive Minor 
Extreme Temperatures Very High High Minor -Serious Minor 
Drought Medium Medium Minor - Serious Minor 
Sources: Resilient MA Plan (Frequency), State Hazard Mitigation Plan 2013 (Severity), HAZUS, Local information. 
Definitions of Hazard Frequency and Severity 
Frequency 
Very low: Very unlikely; minimal examples of historical occurrences. 
Low: Likely to occur at least once by the end of the century; some examples of historical occurrences;
anticipated every 100 years. 
Medium: Likely to occur at least once every 50 years (two or more occurrences in the next century) 
High : Almost certain to occur at least once a year. 
Very High: Almost certain to occur multiple times a year. 
Severity 
Minor : Limited and scattered property damage; limited damage to public infrastructure and essential
services not interrupted; limited injuries or fatalities. 
Serious: Scattered major property damage; some minor infrastructure damage; essential services are
briefly interrupted; some injuries and/or fatalities. 
Extensive: Widespread major property damage; major public infrastructure damage (up to several
days for repairs); essential services are interrupted from several hours to several days; many injuries
and/or fatalities. 
Catastrophic: Property and public infrastructure destroyed; essential services stopped; numerous injuries
and fatalities.

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Not all hazards listed in the Resilient MA Plan affect the Town of Winthrop The Town considered
changing groundwater levels but did not designate that as a hazard in Winthrop. USGS
groundwater monitoring records show no trend in lower groundwater levels over the last 50
years. Further, the Town does not use groundwater wells as a source of water supply, as a
member of the MWRA regional water system. Landslides, while possible, have never occurred 
and the town is ranked “Low Susceptibility” for landslides. Current land use regulations govern 
stabilization of slopes, and the Town did not conclude that further mitigation for landslide is
warranted. 
FLOODING HAZARDS 
FLOODING FROM PRECIPITATION AND COASTAL FLOODING 
Flooding was the most prevalent natural hazard identified by local officials in Winthrop. Given 
the Town’ s location on Boston Harbor, the Town is subject to two kinds of flooding; coastal
flooding, where wind, tide, and storm surges lead to flooding in low-lying areas along the shore
and tidal waterways, and flooding from precipitation, or stormwater flooding, where the rate of
precipitation or amount of stormwater runoff overwhelms the capacity of natural and structured
drainage systems to convey water causing it to overflow the system. These two types of flooding
are often combined as inland flooding is prevented from draining by the push of wind and tide
driven water. 
FLOODING FROM PRECIPITATION 
Flooding is generally caused by severe rainstorms, hurricanes, nor’easters, and thunderstorms. 
Severe rainstorms can occur year-round. Hurricanes are most common in the summer and early fall 
while Nor’easters are most common in winter. Spring snowmelt may exacerbate flooding during 
storm events. Climate change has the potential to exacerbate these issues over time due to
increasing extreme rainfall events. Increase in average annual rainfall may also lead to more
incidents of basement flooding caused by high seasonal groundwater levels. 
Regionally Significant Floods 
There have been a number of major floods that have affected the Metro Boston region over the
last fifty years. Significant historic flood events have included those listed below (NOAA, 2024) 
• The Blizzard of 1978 
• January 1979 
• April 1987 
• October 1991 
• December 1992 
• October 1996 
• June 1998 
• March 2001 
• April 2004 
• May 2006 
• April 2007 
• March 2010 
• December 2010 
• March 2013 
• January 2018 
• March 2018 
• June 2020

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Most severe flooding event within last 15 years 
The most severe flooding event in Eastern Massachusetts in the last 15 years occurred during
March 2010, when a total of 17.7 inches of rainfall was recorded by the Blue Hills Observatory
from three storms over 19 days from March 13 to 31. The weather pattern that consisted of
early springtime prevailing westerly winds that moved three successive storms, combined with
tropical moisture from the Gulf of Mexico, across New England. Torrential rainfall caused March
2010 to be the wettest month on record. 
The March 2010 rainstorms fit the profile of a type of severe precipitation event expected to
increase in frequency as the climate warms. That is, significant precipitation, falling in late
winter as rain rather than snow, on frozen ground, and while vegetation is still dormant. 
One indication of the extent of flooding is the gage height at the nearest USGS streamflow
gauging station, which is on the Saugus River in Saugus, MA. The USGS gage height, shown in
Figure 13, reached 6.41 feet on March 15, 2010 during the first storm, and rose again to 6.21
feet on March 31, 2010 during the second storm. Normal gage height in March is about 3 feet. 
Figure 13- Saugus River Gage Heights, March-April 2010 
Source, US Geological Service, National Water Information System 
Previous Inland/Stormwater Flooding Events 
The best available local data on previous inland flooding events in Winthrop is from NOAA’s 
National Centers for Environmental Information Storm Events Database, which provides county-
level records of natural hazards (see Table 10). Suffolk County, which includes the Town of
Winthrop, experienced 29 flood events from 2005 – 2025. There were no deaths or injuries

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reported and the total reported property damage in the county was $10.945 million dollars.
Damages from the major flooding during the storms of March 2010 totaled $10.7 million.
Notably, that represents 98% of total flood damage for Suffolk County over the entire 20-year
period from 2005 to 2025. The 2010 storms were a federally declared disaster, making federal
assistance available to residents who did not carry flood insurance. That resulted in 25 claims in
the Town of Winthrop, totaling $32,447. The HAZUS analysis estimates flooding damages in
Winthrop from a 100-year storm at $236.8 million and $334.7 from a 500-year storm (Table
46). 
Table 10 Suffolk County Flood Events, 2005 – 2025 
Date Deaths Injuries Property Damage 
5/13/2006 0 0 0 
10/28/2006 0 0 $8,000 
/13/2008 0 0 $5,000 
3/14/2010 0 0 $10,700,000 
8/25/2010 0 0 0 
10/29/2012 0 0 $15,000 
6/7/2013 0 0 0 
9/1/2013 0 0 $5,000 
10/23/2014 0 0 $30,000 
7/23/2016 0 0 0 
7/12/2017 0 0 0 
7/18/2017 0 0 0 
8/2/2017 0 0 0 
9/14/2017 0 0 $25,000 
9/30/2017 0 0 $90,000 
10/30/2017 0 0 0 
5/15/2018 0 0 0 
6/25/2018 0 0 0 
8/12/2018 0 0 $10,000 
9/25/2018 0 0 $3,000 
11/3/2018 0 0 0 
6/29/2019 0 0 $20,00 
7/06/2019 0 0 0 
7/31/2019 0 0 $4,000 
8/7/2019 0 0 0 
6/28/2020 0 0 0 
7/9/2021 0 0 0 
1/23/2023 0 0 0 
7/16/2023 0 0 0 
TOTAL 0 0 $10,945,000 
Source: NOAA, National Centers for Environmental Information

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Probability of Future Events 
Flooding in Winthrop is a high frequency event as defined by the Massachusetts State Hazard
Mitigation Plan. This hazard is almost certain to occur at least once a year. 
Inland Flooding and Climate Change 
Eastern Massachusetts average annual precipitation is 42 inches. While total annual precipitation
has not changed significantly, according to the report When It Rains It Pours – Global Warming
and the Increase in Extreme Precipitation from 1948 to 2011, intense rainstorms and snowstorms
have become more frequent and more severe over the last half century in the northeastern United
States . Extreme downpours are now happening 30 percent more nationwide than in 1948 (see
Figure 14). 
Figure 14 Changes in Frequency of Extreme Downpours, 1948 – 2011 
Source: When It Rains It Pours – Global Warming and the Increase in Extreme 
Precipitation, Environment America Research and Policy Center, July 2012 
Not only are these intense storm events more frequent, they are also more severe; the largest
annual storms now produce 10 percent more precipitation, on average, than in 1948. In
particular, the report finds that New England has experienced the greatest change with intense
rain and snowstorms occurring 85 percent more often than in 1948. 
Data from the 2022 MA Climate Change Assessment related to changes in precipitation patterns
is included in an earlier section of this chapter. Those projections suggest that future rain events
will be increasingly intense and lengthy, which could lead to increased inland and stormwater
flooding. 
Precipitation frequency estimates, which are used to derive stormwater design standards, were
published in 196l by the U.S. Commerce Department in a document known as TP-40 (Technical
Paper 40). The 10-year, 24-hour storm for eastern Massachusetts was calculated as a 4.5-inch

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event. Recently the National Oceanic and Atmospheric Administration published updated
estimates (NOAA Atlas 14), which increased this design storm by 0.6 inches to 5.14 inches for
eastern Massachusetts. Communities should consider future rainfall rates when designing
infrastructure. 
For example, communities could consider using NOAA Atlas 14 rainfall rates with an additional
allowance to account for projected rainfall during the life of projects permitted today when sizing
stormwater infrastructure. DEP takes a similar approach to describe current (not future) rainfall 
rates, called “NOAA14+”. Mystic River Watershed Association (MyRWA) communities propose
“NOAA14++”, which they say reflects 2070 projections. The NOAA 14+ number is calculated by
multiplying the NOAA 14 precipitation frequency estimate upper confidence interval by 0.9 (i.e.,
current but extreme precipitation events reflect 90% of upper confidence intervals). The NOAA
14++ number is the upper confidence interval. A comparison of these numbers is summarized in
Table 11 below (NOAA, 2023) . 
Table 11: Rainfall rates for the 10-year 24-hour storm 
NOAA 14 NOAA 14+ NOAA 14++ 
5.27 inches 5.90 inches 6.56 inches 
NOAA, 2023 
The 2022 MA Climate Change Assessment also highlights the following flooding climate impacts: 
• By 2050, the 1 percent annual chance river flood could be two times more likely to occur 
• By 2090, the historical 10 percent annual chance daily rainfall event (2.8 to 4 inches)
could occur four times more frequently 
• Damage could occur to buildings from heavy rainfall and overwhelmed drainage systems 
• Damage could occur to transit service due to flooding 
• There could be a reduction in the availability of affordably priced housing from direct
damage including from flooding (Commonwealth of Massachusetts, 2022) 
COASTAL FLOODING 
Flooding and coastal storm surges are the primary coastal hazards that lead to the loss of lives or
damage to property and infrastructure in developed coastal areas. Coastal flooding is
associated with severe coastal storms such as Nor’easters and hurricanes which , through the
combination of winds and tides, lead to the inundation of low-lying land areas and damage or
overtopping of seawalls and other coastal infrastructure. Coastal flooding can also be associated 
with routine tidal flooding “King Tides,” or higher astronomic tides. 
Coastal storms are an intricate combination of events that impact a coastal area. Although most
common in the fall and winter seasons, a coastal storm can occur any time of the year and at
varying levels of severity. One of the greatest threats from a coastal storm is flooding due to
storm surge. This is the inundation of land areas along the coastal and estuarine shoreline by
seawaters over and above normal tidal action. Coastal flooding can also be associated with

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routine tidal flooding “King Tides,” or higher astronomic tides. Also, the high tide and storm surge
can limit the ability of stormwater to drain from inland waterways. 
Previous Coastal Flooding Events 
The best available local data for previous coastal flooding occurrences is provided by the NOAA
National Centers for Environmental Information. Suffolk County, which includes the Town of
Winthrop, experienced 37 coastal flood events from 2005 through 2025 (see Table 12). No
deaths or injuries were reported and the total reported property damage in the county was $39
million dollars. 
Table 12 – Suffolk County Coastal Flood/Storm Surges, 2005-2025 
Date Type Deaths Injuries Property Damage 
1/23/2005 Storm Surge 0 0 $100K 
5/24/2005 Storm Surge 0 0 $15K 
5/25/2005 Storm Surge 0 0 $10K 
1/31/2006 Coastal Flood 0 0 $10K 
2/12/2006 Storm Surge 0 0 $15K 
4/15/2007 Coastal Flood 0 0 $5K 
4/16/2007 Coastal Flood 0 0 $5K 
4/17/2007 Coastal Flood 0 0 $10K 
10/18/2009 Coastal Flood 0 0 0 
1/2/2010 Coastal Flood 0 0 0 
3/14/2010 Coastal Flood 0 0 0 
12/27/2010 Coastal Flood 0 0 $50K 
8/27/2011 Storm Surge 0 0 0 
11/23/2011 Coastal Flood 0 0 0 
06/03/2012 Coastal Flood 0 0 0 
06/04/2012 Coastal Flood 0 0 0 
10/29/2012 Coastal Flood 0 0 $3.0M 
2/9/2013 Coastal Flood 0 0 $30.0M 
3/7/2013 Coastal Flood 0 0 00 
1/2/2014 Coastal Flood 0 0 0 
1/3/2014 Coastal Flood 0 0 0 
8/13/2014 Coastal Flood 0 0 0 
10/23/2014 Coastal Flood 0 0 0 
1/27/2015 Coastal Flood 0 0 0 
10/28/2015 Coastal Flood 0 0 0 
1/24/2016 Coastal Flood 0 0 0 
2/8/2016 Coastal Flood 0 0 0 
1/4/2018 Coastal Flood 0 0 $500K 
1/30/2018 Coastal Flood 0 0 $20K 
3/2/2018 Coastal Flood 0 0 0 
10/27/2018 Coastal Flood 0 0 0 
11/25/2018 Coastal Flood 0 0 0 
1/20/2019 Coastal Flood 0 0 0 
10/28/2019 Coastal Flood 0 0 0 
4/3/2020 Coastal Flood 0 0 0 
4/9/2020 Coastal Flood 0 0 0 
9/22/2020 Coastal Flood 0 0 0

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12/17/2020 Coastal Flood 0 0 0 
2/2/2021 Coastal Flood 0 0 0 
7/23/2021 Coastal Flood 0 0 0 
1/17/2022 Coastal Flood 0 0 0 
12/23/2022 Coastal Flood 0 0 0 
1/23/2023 Coastal Flood 0 0 0 
1/10/2024 Coastal Flood 0 0 0 
1/13/2024 Coastal Flood 0 0 0 
3/10/2024 Coastal Flood 0 0 0 
4/4/2024 Coastal Flood 0 0 0 
TOTAL 0 0 $39M 
Source: NOAA, National Centers for Environmental Information 
According to the 2024 Flood Insurance Study for Suffolk County, for the areas of Winthrop that
are impacted by coastal flooding processes, coastal flood hazard analyses were performed by
FEMA to provide estimates of coastal Base Flood Elevations (BFE). Coastal BFEs reflect the
increase in water levels during a flood event due to extreme tides and storm surge as well as
overland wave effects. 
Overland wave hazards were evaluated by FEMA to determine the combined effects of ground
elevation, vegetation, and physical features on overland wave propagation and wave runup.
These analyses were performed at representative transects along all shoreline for which waves
were expected to be present during the floods of the selected recurrence intervals. Table 13
provides the location, stillwater elevations, and starting wave conditions for each Winthrop
transect evaluated for overland wave hazards. The results of these analyses were used to
determine elevations for the 1% annual chance flood. Eight of the Suffolk County transects are in
Winthrop, as shown in Figure 15; these transects are depicted on the FIRM. 
Table 15: Coastal Transect Parameters for Winthrop 
Source: Flood Insurance Study for Suffolk County, 2024

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Figure 15: Suffolk County Shoreline Transect Locations for Winthrop 
Source: Flood Insurance Study for Suffolk County, 2024 
As a peninsula located between Boston Harbor, Belle Isle March, and the Atlantic Ocean,
Winthrop has extensive exposure to coastal flooding along most of its shoreline. Measures of the
severity of coastal flooding include water level elevation and duration of the event. The extent of
flooding in Winthrop is indicated by recorded high water marks documented by the US
Geological Survey for the Blizzard of 1978, the highest coastal flood on record. The USGS, in
cooperation with the Army Corps of Engineers and the Massachusetts Department of Public
Works, inventoried high water marks along the New England coast, including seven locations in
the Town of Winthrop. The high water levels for these locations area summarized in table 14. 
Table 14 High Water Marks in Winthrop, Blizzard of 1978 
Site
No. 
Elevation
(ft-NGVD29) Description 
248 12.45 Lat 42°22'41", long 70058'22", Winthrop, Mass., Winthrop
Beach, good wash line on seventh clapboard from ground at 65
Beach Street, halfway between seventh and eighth clapboard.
Waves over seawall. 
249 7 Lat 42°22'16", long 70°58'12", Winthrop, Mass., Cottage Hill,
good drift line 1.8ft above base of chain link fence across street
from Hadassah Way and Temple Tifreth Israel. Waves over
seawall. 
250 12.67 Lat 42°21'33", long 70°58'16", Winthrop, Mass., Point Shirley,
good to fair debris line 1.8ft above sidewalk on chain link fence
at 965 Bayview on corner. Waves over seawall.

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251 11.04 Lot 42°21'26", long 70°58'16", Point Shirley, Mass., Boston
Harbor, right side" of garage, brick ranch, at 25 Maryland
Avenue. High-water-mark description and elevation furnished
by the Massachusetts Department of Public Works. 
252 11.1 Lat 42°21'27", long 70°58'20", Point Shirley, Mass., Boston
Harbor, foundation and mail box at 80 Otis Street. High-water-
mark description and elevation furnished by the Massachusetts
Department of Public Works. 
253 11.09 Lat 42021'27", long 70°58'20", Point Shirley, Mass., Boston
Harbor, mail box near driveway of 82 Otis Street. High-water-
mark description and elevation furnished by the Massachusetts
Department of Public Works. 
254 10.38 Lat 42°22'06", long 70°58'20", Cottage Hill, Mass., Crystal
Cove, debris line at lower locker deck of Winthrop Yacht Club,
649 Shirley Street. High-water-mark description and elevation
furnished by the Massachusetts Department of Public Works. 
Source: Coastal Flood of Feb. 7, 1978 in ME, MA & NH, Russell A Gadoury, USGS Water Resources
Investigations 79-61 
Probability of Future Occurrence 
Based on the record of previous occurrences coastal flooding events in Winthrop are a high
frequency event as defined by the Resilient MA Plan. This hazard is almost certain to occur at
least once a year. 
Coastal Flooding and Climate Change 
Of all the impacts of climate change, Winthrop is most susceptible to the impacts of sea level
rise, as it will magnify the flooding associated with coastal storms. As shown by records from the
Boston Tide Station (see Figure 11) seas have risen the equivalent of 11 inches over 100 years,
based on monitoring data from 1921. 
The Massachusetts Office of Coastal Zone Management (CZM) adjusted global predictions for
future sea level rise, taking into account local subsidence (see Figure 16). The range of
projections for the future is quite wide, particularly approaching the end of this century. The High
scenario includes ocean warming and a calculation of maximum glacier and ice sheet melt. The
Intermediate High scenario averages higher predictions but includes lesser ice sheet melting. The
Intermediate Low considers lower sea level rise scenarios and limited ice melt. The Historic Trend
reflects a continuation of the current rate of sea level rise. 
The CZM estimate for the Boston Harbor does not take into account more recent research that
suggests the Boston Harbor is included in a region that may experience greater than average
sea level rise. CZM cautions that the Historic and Intermediate Low scenarios may “considerably
underestimate actual sea level rise”, particularly for time horizons beyond 25 years.

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Figure 16 Projected Sea Level Rise for Greater Boston Harbor 
Source: Sea Level Rise: Understanding and Applying Trends and Future Scenarios for Analysis and Planning,
Massachusetts Office of Coastal Zone Management, December 2013. 
Fueled by the warming climate, coastal flooding will become more frequent and severe due to
the combination of sea level rise and more frequent and intense storms. Projections of future sea
level rise identify locations that will be subject to flooding in future years. While those areas do
expand with increasing sea level, the more significant impact will be frequent and deeper
flooding in the locations already subject to coastal flooding. 
Figure 17 shows projections of flood inundation area in Winthrop related to three future sea
level rise scenarios developed for the Massachusetts Coastal Flood Risk Model (MC-FRM) by the
Wood Hole Group. The map shows the extent of flood inundation for a 1% annual chance storm
for projected sea level rise scenarios of 1.2 feet, 2.4 feet, and 4.2 feet. These scenarios are
approximately equivalent to the levels of sea level rise projected for the years 2030, 2050,
and 2070, respectively. This map is also included in the hazard map series in Appendix A.

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Figure 17: Areas Inundated in Future Sea Level Rise Scenarios 
Source: Woods Hole Group, Massachusetts Coastal Flood Risk Model

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INLAND AND COASTAL FLOOD HAZARD AREAS IN WINTHROP 
Information on potential flood hazard areas was taken from two sources. The first was the
National Flood Insurance Rate Maps. The FIRM flood zones are shown on Map 3 in Appendix A
and their definitions are listed below. The most significant areas of Zone A (1% annual chance of
flooding) are across the Belle Isle Marsh and Winthrop’s shoreline, both facing the Atlantic Ocean 
and Boston Harbor, with the most extensive areas on the ocean side. There are no flood hazard 
areas in Winthrop associated with rivers and streams; all of the town’s exposure to flooding is 
from coastal sources. 
Locally Identified Areas of Inland and Coastal Flooding 
The second source of information on local flooding was the Winthrop Hazard Mitigation Team.
The locally identified areas of flooding described below were identified by town staff as areas
where flooding occurs. 
The 15 locally identified areas of flood hazard described below and shown on Map 8 in
Appendix A were identified by the Winthrop Hazard Mitigation Team as areas where flooding
is known to occur. Sites 12 through 15 were added to the plan for this 2025 update. These
areas do not necessarily coincide with the flood zones from the FIRM maps. They may be areas
that flood due to inadequate drainage systems or other local conditions rather than location
within a flood zone, or areas subject to coastal flooding in part due to infrastructure that may
require upgrading. The site numbers correspond to the numbers on Map 8, “Hazard Areas”. The 
numbers do not reflect priority order. 
Flood Insurance Rate Map Zone Definitions 
Zone A (1% annual chance): Zone A is the flood insurance rate zone that corresponds to the
100-year floodplains that are determined in the Flood Insurance Study (FIS) by
approximate methods. Because detailed hydraulic analyses are not performed for such
areas, no BFEs (base flood elevations) or depths are shown within this zone. Mandatory
flood insurance purchase requirements apply. 
Zone AE and A1-A30 (1% annual chance): Zones AE and A1-A30 are the flood insurance
rate zones that correspond to the 100-year floodplains that are determined in the FIS by
detailed methods. In most instances, BFEs derived from the detailed hydraulic analyses are
shown at selected intervals within this zone. Mandatory flood insurance purchase
requirements apply. 
Zone X500 (0.2% annual chance) : Zone X500 is the flood insurance rate zone that
corresponds to the 500-year floodplains that are determined in the Flood Insurance Study
(FIS) by approximate methods. Because detailed hydraulic analyses are not performed for
such areas, no BFEs (base flood elevations) or depths are shown within this zone. 
Zone VE (1% annual chance): Zone VE is the flood insurance rate zone that corresponds to
the 100-year coastal floodplains that have additional hazards associated with storm waves.
BFEs derived from the detailed hydraulic analyses are shown at selected intervals within this
zone . Mandatory flood insurance purchase requirements apply.

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Locally Identified Areas of Flooding 
1) Yirrell Beach: coastal surge and flooding during storm events 
2) Shirley Street Neighborhood: low-lying street area and adjacent seawall experience wave
overtopping and flooding during storm events 
3) Lewis Lake: Serves as drainage area for large part of downtown area. Lake overflows during
storm events and causes flooding in adjacent areas. 
4) Ingleside Park: Backup and flooding due to lack of storm water storage capacity and
undersized drains. Floods during high tide events coinciding with high precipitation events of
greater than 1 inch. 
5) Lower Nahant Avenue: coastal surge, high tide and high precipitation events all cause backup in
undersized drain lines and flooding within the adjacent neighborhood. 
6A) Woodside seawall and headwall on Boston Harbor: coastal surge flooding during storm events 
6B) Somerset seawall and headwall on Boston Harbor: coastal surge flooding during storm events. 
6C) Sargent Street seawall and headwall on Boston Harbor: coastal surge flooding during storm
events. 
6D) Cottage Park seawall and headwall on Boston Harbor: coastal surge flooding during storm
events. 
7) Coughlin Park: coastal erosion and flooding during higher northwest wind events and coastal
storms. 
8) Bayou Street Neighborhood- flooding due to undersized drainage line that backs up in high
precipitation events. 
12)Pico Avenue off of Sunnyside – seawall needs to be raised for 13-foot tide. 
13) Morton Street and Banks. 
14) Washington Street and River Road – floods during every large rain event. 
15) Pleasant Street and Girdlestone Road – low-lying area floods, 
The area of Winthrop that floods the most frequently is Point Shirley. In addition to the eastern
side of Point Shirley being directly impacted by ocean waves and storm surge, the western side
of the Point is often impacted by the what local residents desc ribe as the “Boston Harbor
bathroom effect” in which tidal driven storm surge causes water build -up in the Harbor and
causes flooding on the western side of Point Shirley. Another area that floods frequently is the
residential area surrounding Lewis Lake. Lewis Lake drains approximately half of the Town.
Homes in this area flood because the lake is silted up which reduces its capacity.

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Flooding also occurs in the vicinity of Ingleside Park. The park is at sea level with a pipe that
drains to the bay. There is a valve that shuts during heavy tides but the area may need a pump
station as well. To help with flooding in this area, the Town has constructed dikes around two
homes as a temporary solution. The south end of Yirrell Beach, in the vicinity of Wyman Street
also experiences flooding because the seawall does not extend far enough. The road leading to
the MWRA Deer Island wastewater facility is also prone to flooding during larger storm events. 
The seawall at Yirrell Beach to Deer Island remains one of the Town’s top priorit y hazard mitigation
measures. This seawall is occasionally breached which results in sand coming up over the wall.
Because the seawall ends at Wyman Street, this street floods, which can affect up to 40 homes. In
2003 the Town had to remove four feet of gravel that had washed up on Wyman Street. 
Repetitive Loss and Severe Repetitive Loss Properties 
As defined by the National Flood Insurance Program (NFIP), a repetitive loss property is any
property which the NFIP has paid two or more flood claims of $1,000 or more in any given 10-
year period since 1978. A Severe Repetitive Loss property consists of any NFIP-insured
residential property that has met at least one of the following flood loss criteria since 1978: 
• 4 or more separate claim payments of more than $5,000 each (including building and 
contents payments); or 
• 2 or more separate claim payments (building payments only) where the total of the 
payments exceeds the current value of the property. 
There are 153 repetitive loss properties in Winthrop. These properties had a total of 489 losses,
totaling $ 3,772,415 in building and contents damages. In addition there are 11 Severe Repetitive
Loss properties that have had 11 losses totaling $654,231 . The total of all losses for RL and SRL
properties in Winthrop is $ 4,426,646. Table 15 summarizes the number of repetitive loss and
severe repetitive loss properties in Winthrop and the number of losses and insurance payments
for building losses and building contents losses. 
Table 15. Summary of Repetitive Losses and Claims 
Repetitive Loss
Properties 
Severe Repetitive
Loss Properties Total 
Number of Properties 153 11 164 
Number of Losses 489 63 552 
Building Claim Payments $3,476,995 $588,955 $4,065,950 
Contents Claim Payments $294,777 $65,202 $359,979 
Total Claim Payments $3,772,415 $654,231 $4,426,646 
Source: Massachusetts Emergency Management Agency

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COASTAL EROSION 
Coastal shorelines change constantly in response to storms, seasons, sea level, and human
alterations. Rising seas and more frequent and intense storms will tend to increase erosion,
although some areas may actually accrete material due to localized variation in coastal
dynamics. The severity of erosion is related to such factors as exposure to high energy waves,
sediment size, sea level rise, near-shore bathymetry, and human interference with sediment
supply. 
Coastal landforms such as coastal banks are essential to maintaining a supply of sediment to
beaches and dunes. Where engineered structures are used to stabilize shorelines, the natural
process of erosion is interrupted, decreasing the amount of sediment available and causing
erosion to adjacent areas. Under conditions of reduced sediment, the ability of coastal resource
areas such as dunes and beaches to provide storm damage prevention and flood control benefits
is continually reduced. A major challenge is to ensure that regional sediment supplies are
managed effectively and in ways that allow the beneficial storm damage prevention and flood
control functions of natural coastal processes to continue — both for future projects and, where
possible, existing coastal development. 
In Winthrop, there are many examples of both public and private infrastructure that are
impacting sediment supplies to beaches. One area is the seawall along Winthrop Shore Drive and
another is the private seawall along both sides of Shirley Street. Other areas with hard
engineered infrastructure that may be impacting the supply of sediment to coastal beaches
include Brewster and Grandview Avenues, Faunbar Avenue and Terrace Avenue. 
Coastal Erosion and Shoreline Change 
Coastal shorelines change constantly in response to wind, waves, tides, sea level fluctuation,
seasonal and climatic variations, human alteration, and other factors that influence the movement
of sand and material within a shoreline system. The loss (erosion) and gain (accretion) of coastal
land is a visible result of the way shorelines are reshaped in the face of these dynamic conditions.
Shorelines tend to change seasonally, accreting slowly during the summer months when sediments
are deposited by relatively low energy waves and eroding dramatically during the winter when
sediments are moved offshore by high-energy storm waves, such as those generated by 
nor’easters. Regardless of the season, coastal storms typically cause erosion. 
Coastal erosion and shoreline change can result in significant economic loss through the destruction
of buildings, roads, infrastructure, natural resources, and wildlife habitats. Damage often results
from the combination of an episodic event with severe storm waves and dune or bluff erosion. 
Some of the methods used by property owners to stop, or slow down, coastal erosion or shoreline
change can actually exacerbate the problem. Attempting to halt the natural process of erosion
with seawalls and other hard structures typically worsens the erosion in front of the structure,
prevents any sediment behind the structure from supplying down drift properties with sediment
and subjects down drift beaches to increased erosion. Without the sediment transport associated
with erosion, some of the Commonwe alth’s and Winthrop’s greatest assets and attractions – 
beaches, dunes, barrier beaches, salt marshes, and estuaries are threatened and could be slowly
diminished as the sediment sources that feed and sustain them are eliminated.

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Extent and Previous Occurrences 
The Massachusetts Coastal Erosion Commission published an assessment of coastal erosion in
2015. A shoreline characterization project was implemented to categorize the land uses and
natural resources potentially at risk from coastal erosion. The results of the characterization
provide a baseline from which to monitor and identify landscape-level trends and patterns for
evaluating adaptation and hazard mitigation strategies for a particular location or region. 
The Commission assessed the trends of coastal erosion by examining the results of the
Massachusetts Shoreline Change Project and providing a summary assessment of past shoreline
changes. Launched in 1989, the Shoreline Change Project analyzed data from historical and
modern sources, mapping local high water line and developing shoreline change rates over both
a long-term period (from the mid-1800s to 2009) and a short-term period (from 1970-2009)
These data provide insight into the historical migration of the shoreline and erosional hot spots. 
The results of the shoreline characterization were used to analyze shoreline change rates for
Winthrop, including long-term and short-term erosion and accretion trends The analysis took into
account various types of shoreline, which are displayed in Figure 18, showing the percent of each
type. 
Figure 18: Percent of Assessed Shoreline by Type 
Source: Report of the Mass. Coastal Erosion Commission, 2015 
The rates of shoreline erosion or accretion for Winthrop are shown in Table 16. The long-
term accretion rate since the mid- 1800’s was 0.4 feet/year. The short-term accretion rate
from 1970 to 2009 was the same. 
Table 16: Average shoreline change and Uncertainty 
Source: Report of the Mass. Coastal Erosion Commission, 2015

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Table 17 shows both long-term and short-term rates of change for three types of shoreline in
Winthrop. The highest rate of accretion is associated with Beach, over long-term. The erosion
rates for Bank ranged from -0.10 feet/year short-term to 0.15 feet/year In the long-term. 
Table 17 Average shoreline change by shoreline type 
Source: Report of the Mass. Coastal Erosion Commission, 2015 
CZM Coastal Erosion Viewer 
Massachusetts Coastal Zone Management (MA CZM) in cooperation with the U. S. Geological
Survey (USGS) provides shoreline change data for the Massachusetts coast. The most recently
available data provide long- term (1800’s – 2014) and short-term (1970-2014) data. The
analysis for Winthrop shows somewhat different patterns of erosion from the long-term to the
short-term records. see Figures 19A and 19B). This illustrates the effects of climate trends along
some parts of the shoreline, as erosion rates in some areas have generally increased since the
19 th and 20 th centuries. 
The CZM Coastal Erosion Viewer provides more detailed views of historic shoreline changes
along a series of transects of the shoreline. A detailed transects for Winthrop is shown in Figure
20. The yellow transects indicate no statistical change while the red transects indicate net
shoreline loss . This is the section of Winthrop’s shoreline that has experienced the most significant 
change. 
Coastal Erosion and Climate Change 
As sea level continues to rise, coastal erosion will increase over time most likely with increasing
frequency and severity. This represents a significant long-term hazard for the Town of Winthrop.

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Figure 19A: Long-Term Coastal Erosion in Winthrop, 1840s-2018 
Source : MA Coastal Zone Management, Coastal Erosion Viewer

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Figure 19B: Short-Term Coastal Erosion in Winthrop, 1970-2019 
Source : MA Coastal Zone Management, Coastal Erosion Viewer

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Figure 20: Winthrop Shoreline Change (1847-2008) 
Source : MA Coastal Zone Management, Coastal Erosion Viewer

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TSUNAMIS 
A tsunami is a surge of ocean water typically caused by an offshore earthquake. FEMA defines
tsunami as a series of large seismic sea waves created by an underwater disturbance caused by
geologic activity such as earthquakes, volcanic eruptions, or underwater landslides. The severity of
a tsunami is related to its wave height at the shore, and the extent of runup. Tsunami wave action
over the shore is variable and mainly dependent of the combination of both submarine and land
topography and the orientation of the arriving waves. The extent of damage and impact from
tsunami depends upon the source and severity of onset on the tide cycle. Coastal areas that are
potentially at greater risk are less than 25 feet above sea level and within a mile of the
shoreline. As such, Winthrop would be considered vulnerable to coastal inundation from tsunami.
While all of the coast of Massachusetts could potentially be subject to a tsunami, Massachusetts
has never experienced a significant tsunami. 
Probability of Future Occurrence 
According to the West Coast and Alaska Tsunami Warning Center, an Atlantic based tsunami
threat level for the US Atlantic coast is low when compared to the Pacific and Caribbean coasts.
Geophysics specialists from the U.S. Geologic Survey and the Woods Hole Oceanographic
Institute have researched the Georges Bank Lower Slope of the North Atlantic Ocean and the
relationship between submarine landslides and earthquakes (see Figure 21). 
Figure 21 - Atlantic Based Tsunami- Potential Threat 
T he most likely source would be a landslide that happens underwater about 215 miles offshore in
an area known as the Continental Slope. The US Geologic Survey has researched the probability
of a landslide on the Continental Shelf, and the likelihood that a tsunami will hit the Atlantic coast

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is considered to be fairly low. Based on the record of previous occurrences, Tsunami in Winthrop
is a Very Low frequency event as defined by the Resilient MA Plan 
Tsunamis and Climate Change 
Unlike most other coastal hazards, Tsunamis are events driven by geological processes, principally
earthquakes and undersea landslides, which are not likely to be related to climate change.
However. according to the Resilient MA Plan, collapse of glaciers resulting from a warming
climate could cause landslides that could generate tsunamis more powerful than those caused by
earthquakes. 
DAM HAZARDS 
Dam failure can occur as a result of structural failure, independent of a hazard event, or as the
result of the impacts of a hazard event such as flooding associated with storms or an earthquake.
In the event of a dam failure, the energy of the water stored behind even a small dam can cause
loss of life and property damage if there are people or buildings downstream. The number of
fatalities from a dam failure depends on the amount of warning provided to the population and
the number of people in the area in the path of the dam’s floodwaters. 
Dam failure is a highly infrequent occurrence, but a severe incident could result in loss of lives and
significant property damage. Since 1984, three dams have failed in or very near to
Massachusetts, one of which resulted in a death . 
There are no publicly or privately owned dams in Winthrop listed by the Department of
Conservation Dam Safety Office. 
HURRICANES AND TROPICAL STORMS 
Wind-related hazards include hurricanes, tropical storms, and tornadoes as well as high winds 
during Nor’easters and thunderstorms. Information on wind related hazards can be found on Map 
5 in Appendix A, which indicates that the 100-year wind speed in Winthrop is 110 miles per
hour. 
Hurricanes begin as tropical storms over the warm moist waters of the Atlantic, off the coast of
West Africa near the equator. As the moisture evaporates, it rises until enormous amounts of
heated, moist air are twisted high in the atmosphere. The winds begin to circle counterclockwise
north of the equator or clockwise south of the equator. The center of the hurricane is called the
eye. 
Tropical cyclones (Tropical Depressions, Tropical Storms, and Hurricanes) form over the warm,
moist waters of the Atlantic, Caribbean, and Gulf of Mexico. When water temperatures are at
least 80° F, hurricanes can grow and thrive, generating enormous amounts of energy, which is
released in the form of numerous thunderstorms, flooding rainfall, and, very damaging winds.

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The damaging winds help create a dangerous storm surge (rise in the water above the normal
astronomical tide). 
A Tropical Depression is declared when there is a low pressure center in the tropics with sustained
winds of 25-33 mph. A Tropical Storm, which is given a name, is defined as having sustained
winds from 34-73 mph. If sustained winds reach 74 mph or greater, it becomes a Hurricane. 
Hurricanes can range from compact storms only 50 miles across, to huge storms, as much as 500
miles wide -- Hurricane Allen in 1980 took up the entire Gulf of Mexico. There generally are two
source regions for the storms that have the potential to strike New England: 1) off the Cape
Verde Islands near the west coast of Africa and 2) in the Bahamas. The Cape Verde storms tend
to be very large in diameter, since they have a week or more to traverse the Atlantic Ocean and 
grow. Bahamas’ storms tend to be sma ller, but they can also be just as powerful and their effects
can reach New England in only a day or two. 
A hurricane is strongest as it travels over the ocean and is particularly destructive to coastal
property as the storm hits the land. The Town's entire area is vulnerable to hurricanes. Hurricanes
occur between June and November. 
Hurricane intensity is measured according to the Saffir/Simpson scale, which categorizes hurricane
intensity linearly based upon maximum sustained winds, barometric pressure, and storm surge
potential. These are combined to estimate potential damage. The following gives an overview of
the wind speeds, surges, and range of damage caused by different hurricane categories: 
Scale No. (Category) Winds(mph) Storm Surge (ft) Potential 
Damage 
1 74 – 95 4 - 5 Minimal 
2 96 – 110 6 - 8 Moderate 
3 111 – 130 9 - 12 Extensive 
4 131 – 155 13 - 18 Extreme 
5 > 155 >18 Catastrophic 
Source: NOAA 
Previous Occurrences 
Since 1900, 39 tropical storms have impacted New England (NESEC). Massachusetts has
experienced approximately 32 tropical storms, nine Category 1 hurricanes, five Category 2
hurricanes and one Category 3 hurricane. A hurricane or storm track is the line that delineates the
path of the eye of a hurricane or tropical storm. 
A hurricane or tropical storm track is the line that delineates the path of the eye of the hurricane
or storm. As shown in Map 5 in Appendix A, no hurricanes or tropical storms have tracked directly
over Winthrop, but several passed very close to the town, one in 1902, and two more in 1923.
However, hurricanes have regional impacts, and Winthrop experiences the impacts of hurricanes
and tropical storms regardless of whether the storm track passes directly through the Town. Storms
that track west of the town result in stronger winds, while those that pass to the east may bring

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more rainfall. Numerous hurricanes have affected the communities of eastern Massachusetts over
the last century(see Table 18). 
Table 18 Hurricane Records for Massachusetts, 1908 - 2025 
Hurricane Event Date 
Hurricane of 1908 May 24-31, 1908 
Hurricane of 1915 July 31, 1915 
Hurricane of 1916 July 10-22, 1916 
Great New England Hurricane September 21, 1938 
Great Atlantic Hurricane September 14-15, 1944 
Hurricane Doug September 11-12, 1950 
Hurricane Carol August 31, 1954 
Hurricane Edna September 11, 1954 
Hurricane Diane August 17-19, 1955 
Hurricane Donna September 12, 1960 
Hurricane Gloria September 27, 1985 
Hurricane Bob August 19, 1991 
Hurricane Bertha July 5 - 17, 1996 
Hurricane Hanna August 28, 2008 
Hurricane Earl September 4, 2010 
Tropical Storm Irene August 28, 2011 
Hurricane Sandy October 29-30, 2012 
Source: National Oceanic and Atmospheric Administration 
The two most recent hurricanes, Irene from August 21 – 30, 2011and Sandy from October 22 – 31,
2012 fortunately did not track directly over Winthrop). Hurricane Sandy was a Category 3
hurricane at its peak intensity and weakened to a Category 2 off the northeastern Atlantic coast.
Hurricane Sandy became the largest Atlantic hurricane on record with winds spanning 1,100
miles. Strong tropical force winds from the northeast quadrant of the post tropical cyclone, Sandy 
developed into a super storm nor’easter that impacted Winthrop and Suffolk County (Figure 22). 
Winthrop closed the tidal gate on Winthrop Shore Drive at 7 A.M. on the morning of Sandy’s 
arrival. 
News reports for Hurricane Sandy indicated key findings, as reported by the Winthrop Transcript 
on November 1, 2012: “(Fire Chief) Flanagan said there was some personal property damage 
such as electrical services being dismantled from homes and four boats breaking loose in the
harbor. The chief also reported that at the peak of the storm 2,100 customers were without
electrical power. 
The Winthrop Fire Department staged fire apparatus and ambulances on Point Shirley during
periods of high tides. Shirley Street at Tewksbury Street became impassable for a period of a 
few hours during Monday morning’s high tide. The chief also said that tw o telephone poles went
down on Putnam Street while another pole broke off at the base on Veterans Road. At 10 a.m. on
Monday, Flanagan had the Medical Reserve Corps (MRC) open a shelter at the Cummings School 
in case of tidal concerns.”

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Figure 22: Winthrop Shore Drive, October 28, 2012, Hurricane Sandy 
Photo: courtesy of Winthrop Transcript 
Hurricanes typically have regional impacts beyond their immediate tracks. Falling trees and
branches are a significant problem because they can result in power outages when they fall on
power lines or block traffic and emergency routes. Hurricanes are a town-wide hazard in
Winthrop. Potential hurricane damages to Winthrop have been estimated using HAZUS-MH. Total
damages are estimated at $7.2 million for a100-year frequency hurricane and $30.9 million for
a 500-year frequency hurricane. Other potential impacts such as debris and evacuation needs
are detailed in Table xx. 
Probability of Future Occurrence 
Based on records of previous occurrences, hurricanes in Winthrop are a medium frequency event
as defined by the Resilient MA Plan. This hazard occurs from once in 5 years to once in 50 years,
or a 2% to 20% chance per year. 
Hurricanes and Climate Change 
Climate models suggest that hurricanes and tropical storms will become more intense as warmer
ocean waters provide more fuel for the storms. In addition, rainfall amounts associated with
hurricanes are predicted to increase because warmer air can hold more water vapor 
TORNADOES 
A tornado is a violent windstorm characterized by a twisting, funnel-shaped cloud. These events
are spawned by thunderstorms and occasionally by hurricanes and may occur singularly or in
multiples. T hey develop when cool air overrides a layer of warm air, causing the warm air to rise
rapidly. Most vortices remain suspended in the atmosphere. Should they touch down, they become
a force of destruction. Some ingredients for tornado formation include:

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• Very strong winds in the mid and upper levels of the atmosphere 
• Clockwise turning of the wind with height (from southeast at the surface to west aloft) 
• Increasing wind speed with altitude in the lowest 10,000 feet of the atmosphere (i.e., 20
mph at the surface and 50 mph at 7,000 feet.) 
• Very warm, moist air near the ground with unusually cooler air aloft 
• A forcing mechanism such as a cold front or leftover weather boundary from previous
shower or thunderstorm activity 
Tornado damage severity is measured by the Fujita Tornado Scale, in which wind speed is not
measured directly but rather estimated from the amount of damage. As of February 01, 2007,
the National Weather Service began rating tornados using the Enhanced Fujita-scale (EF-scale). It
is considerably more complicated than the original F-scale, and it allows surveyors to create more
precise assessments of tornado severity. The EF-scale is summarized in Table 19. 
Table 19: Enhanced Fujita Scale 
Source: SHMCAP 2018

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The frequency of tornadoes in eastern Massachusetts is relatively low; on average, there are six
tornadoes that touchdown somewhere in the Northeast region every year. The strongest tornado
in Massachusetts history was the Worcester Tornado in 1953 (NESEC). 
The most recent significant tornado event in Massachusetts was in Springfield in 2011. This
tornado caused significant damage and resulted in 4 deaths in June of 2011. Although there
have been no recorded tornadoes within the Town of Winthrop, a tornado struck nearby Chelsea
and Revere in 2014. The tornado touched down in Chelsea just south of Route 16 and moved
north into R evere’s business district along Broadway and ended near the intersection of Routes 1
and 60. The path was approximately two miles long and 3/8 mile wide, with wind speeds up to
120 miles per hour. Figure 23 shows the tornado’s track in Chelea and Revere and illustrates its 
proximity to Winthrop. This is the only tornado recorded for Suffolk County from 1950 to 2025. 
This tornado resulted in $4 million in damage, two injuries, and no fatalities , as summarized in
Table 20. Most of the damage was rated EF-1, but EF-2 rated damage did occur near Revere
Beach Parkway. Windows were blown out of Revere City Hall and the roof was damaged. Sixty-
four structures sustained damage that ranged from siding torn off to roofs lifted or blown off.
Thirteen of these structures were deemed uninhabitable.. Trees fell on cars, a few of these
crushed. Revere High School also sustained damage. Police reported a car that had been
overturned at the intersection of Revere Street and Carleton Avenue. Near the rotary at Route 60
and Broadway, a billboard was blown onto several cars. The city set up a shelter at a local
school for displaced residents. National Grid reported that 3,000 homes were without power. 
Figure 23 – Chelsea/Revere Tornado of 2014 
Source: National Centers for Environmental Information

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Table 20 - Tornado Records for Suffolk County 
Date Fujita Fatalities Injuries Damage 
70/28/2014 EF2 0 2 $4,000,000 
Source: National Centers for Environmental Information 
Buildings constructed prior to current building codes may be somewhat more vulnerable to
damages caused by tornadoes. Evacuation of impacted areas may be required on short notice.
Sheltering and mass feeding efforts may be required along with debris clearance, search and
rescue, and emergency fire and medical services. Key routes may be blocked by downed trees
and other debris, which in Winthrop could be a significant hazard since there are only two routes
connecting the Town to the mainland. Power outages are also typically associated with tornadoes. 
Although tornadoes are a potential Town-wide hazard in Winthrop, tornado impacts are
relatively localized compared to severe storms and hurricanes, as the Rever tornado illustrates.
Damages from any tornado in Winthrop would greatly depend on the track of the tornado.
Generally, the more densely developed areas in the northern part of town could sustain more
building damage in the event of a tornado in Winthrop. 
Probability of Future Occurrence 
Based on the record of previous occurrences since 1950, Tornado events in Winthrop are a Low
frequency event as defined by the Resilient MA Plan. This hazard is likely to occur at least once
by the end of the century. 
Tornadoes and Climate Change 
According to the Resilient MA Plan, it is possible that severe thunderstorms which can include
tornadoes may increase in frequency and intensity. However, scientists have less confidence in the
models that seek to project future changes in tornado activity. The Massachusetts 2022 Climate
Change Assessment does not include information related to tornadoes. 
SEVERE WINTER STORMS (NOR’EASTERS / BLIZZARDS) 
Winter storms, including nor’easters, heavy snow, blizzards, and ice storms, are the most common 
and most familiar of the region’s hazards that affect large geographic areas. The majority of 
blizzards and ice storms in the region cause more inconvenience than serious property damage,
injuries, or deaths. However, periodically, a storm will occur which is a true disaster, and
necessitates intense large-scale emergency response. The strongest among these are typically 
nor’easters. 
NOR’EASTER S 
A northeast coastal storm, known as a nor’easter, is typically a large counterclockwise wind
circulation around a low-pressure center. Featuring strong northeasterly winds blowing in from the 
ocean over coastal areas, nor’easters are relatively common in the winter months in New England 
occurring one to two times a year. The storm radius of a nor’easter can be as much as 1,000 miles 
and these storms feature sustained winds of 20 to 40 mph with gusts of up to 70 mph (Figure 24).
These storms are accompanied by heavy rains or snows, depending on temperatures.

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Figure 24 – Nor’easter Satellite Image 
Source: The Geostationary Operational Environmental Satellite Program (GOES), 
A joint effort of NASA and NOAA.. 
The Dolan- Davis classification system for Nor’easters was developed to complement the Saffir - 
Simpson scale used for hurricanes. The scale is based on mean wave height caused by the Nor’easter
– different from the Saffir-Simpson classification of hurricanes based on wind speed. The scale was 
developed using data from 1,347 Nor’easters over a forty-year time frame. Robert Dolan and 
Robert Davis developed the scale to classify Nor’easters from Class I through Class V. Table 21
below summarizes each class of storm. 
Table 21. Dolan- Davis Classification System for Nor’easters 
Storm Class Mean Wave Height (m) Beach Erosion Property Damage 
Class I (weak) 2.0 Minor None 
Class II (moderate) 2.5 Moderate None 
Class III (significant) 3.2 Extends across beach Moderate 
Class IV (severe) 5.0 Severe with recession Loss of structures at community
scale 
Class V (extreme) 6.8 Extreme Extensive regional scale losses in
millions of dollars 
Landsea, C. (2009, February 6). FAQ: Hurricanes, Typhoons, and Tropical Cyclones and Williams, J. (2005, May 17). Hurricane scale invented to
communicate storm danger. 
Previous occurrences of nor’easters include the storm events included in Table 22. Many of the 
historic flood events identified in the previous section were precipitated by nor’easters, including
the “Perfect Storm” event in 1991. More recently, large nor’easters in 2015 and 2018 caused
significant damage across the coast.

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Table 22 : Nor’easter Events for Massachusetts, 1978 - 2024 
Date Nor’easter Event 
February 1978 Blizzard of 1978 
October 1991 Severe Coastal Storm (“Perfect Storm”) 
December 1992 Great Nor’easter of 1992 
January 2005 Blizzard/Nor’easter 
October 2005 Coastal Storm/Nor’easter 
April 2007 Severe Storms, Inland & Coastal Flooding/Nor’easter 
January 2011 Winter Storm/Nor’easter 
October 2011 Severe Storm/Nor’easter 
February 2013 Blizzard of 2013 
January 2015 Blizzard of 2015 
March 2015 March 2015 Nor’easters 
January 2018 January 2018 
March 2018 March 2018 
Winthrop is vulnerable to both the wind and precipitation that accompanies nor’easters. High 
winds can cause damage to structures, fallen trees, and downed power lines leading to power
outages. Intense rainfall can overwhelm drainage systems causing localized flooding of streets as
well as localized flooding of residential and business structures. Fallen tree limbs as well as heavy
snow accumulation and intense rainfall can impede local transportation corridors, and block
access for emergency vehicles. Due to its location on the coast, the entire Town is at risk from the 
wind, rain or snow impacts from a nor’easter, depending on the track and radius of the storm . 
Based on the record of previous occurrences, nor’easters in Winthrop are high frequency events
as defined by the Resilient MA Plan. This hazard is almost certain to occur at least once a year. 
BLIZZARDS & HEAVY SNOW 
Winter storms are a combination hazard because they often involve wind, ice, and heavy snow 
fall. The National Weather Service defines “heavy snow fall” as an event generating at least four 
inches of snowfall within a 12-hour period (NOAA, 2009). Blizzards and winter storms are often 
associated with a nor’easter event (see nor’easters section above). 
A blizzard is a winter snowstorm with sustained or frequent wind gusts to 35 mph or more,
accompanied by falling or blowing snow which reduces visibility to or below ¼ mile. These
conditions must be the predominant conditions over a three-hour period. Extremely cold
temperatures are often associated with blizzard conditions but are not a formal part of the
definition. The hazard related to the combination of snow, wind, and low visibility significantly
increases when temperatures drop below 20 degrees.

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The Regional Snowfall Index (RSI) characterizes and ranks the severity of northeast snowstorms.
RSI has five categories: Extreme, Crippling, Major, Significant, and Notable. RSI scores are a
function of the area affected by the storm, the amount of snow, and the number of people living
in the path of the storm. The largest RSI values result from storms producing heavy snowfall over
large areas that include major metropolitan centers. The RSI categories are shown in Table 23. 
Table 23: Regional Snowfall Index 
Category RSI Value Description 
1 1 – 3 Notable 
2 3-6 Significant 
3 6-10 Major 
4 10-18 Crippling 
5 18+ Extreme 
Source: 2018 SHMCAP 
The best available local data on past occurrences and impacts of winter storm events are
reported for Suffolk County by the National Centers for Environmental Information (NCEI). From
2010 through 2024, Suffolk County experienced 51 winter storm events, including three
blizzards, resulting in one injury, no deaths, and $703,100 in property damage, as shown in
Table 24. 
Table 24: Winter Storms, Heavy Snow and Blizzards
in Suffolk County, 2010 - 2024 
Date Event Deaths Injuries Property Damage ($) 
12/26/2010 Winter Storm 0 0 0 
1/12/2011 Winter Storm 0 0 50000 
1/21/2011 Winter Storm 0 0 0 
1/26/2011 Heavy Snow 0 0 0 
2/1/2011 Winter Storm 0 0 432000 
1/21/2012 Winter Storm 0 0 0 
2/8/2013 Heavy Snow 0 0 0 
2/8/2013 Blizzard 0 0 0 
2/17/2013 Winter Storm 0 0 0 
3/7/2013 Heavy Snow 0 0 0 
3/18/2013 Heavy Snow 0 0 0 
12/17/2013 Heavy Snow 0 0 0 
1/2/2014 Heavy Snow 0 0 0 
2/5/2014 Heavy Snow 0 0 0 
1/24/2015 Heavy Snow 0 0 0 
1/26/2015 Blizzard 0 0 0 
2/2/2015 Heavy Snow 0 0 0 
2/8/2015 Heavy Snow 0 0 0 
2/14/2015 Heavy Snow 0 0 0

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1/23/2016 Heavy Snow 0 0 0 
2/5/2016 Heavy Snow 0 0 10000 
2/8/2016 Heavy Snow 0 0 0 
3/21/2016 Winter Storm 0 0 0 
4/4/2016 Winter Storm 0 0 0 
12/17/2016 Winter Storm 0 0 0 
1/7/2017 Winter Storm 0 0 0 
2/8/2017 Winter Storm 0 0 150000 
2/9/2017 Winter Storm 0 0 0 
3/14/2017 Heavy Snow 0 0 0 
12/9/2017 Winter Storm 0 0 0 
12/22/2017 Winter Storm 0 1 5000 
12/25/2017 Winter Storm 0 0 2000 
1/4/2018 Winter Storm 0 0 0 
2/7/2018 Winter Storm 0 0 40000 
2/17/2018 Winter Storm 0 0 0 
3/7/2018 Winter Storm 0 0 0 
3/13/2018 Blizzard 0 0 10000 
1/19/2019 Winter Storm 0 0 0 
2/18/2019 Winter Storm 0 0 0 
3/3/2019 Winter Storm 0 0 0 
10/30/2020 Winter Storm 0 0 2000 
12/16/2020 Heavy Snow 0 0 0 
2/7/2021 Heavy Snow 0 0 0 
1/7/2022 Heavy Snow 0 0 0 
1/28/2022 Heavy Snow 0 0 500 
2/25/2022 Heavy Snow 0 0 0 
1/20/2023 Heavy Snow 0 0 0 
1/23/2023 Heavy Snow 0 0 600 
2/23/2023 Heavy Snow 0 0 0 
3/3/2023 Heavy Snow 0 0 0 
3/14/2023 Heavy Snow 0 0 1000 
TOTAL 0 1 $703,100 
Source: NOAA, National Centers for Environmental Information 
Another indication of previous severe winter events is the list of Presidentially declared disasters
for blizzards and snowstorms. There have been 14 in Massachusetts since 1978, as shown in Table
25. The most significant single winter storm was the “Blizzard of 1978,” which resulted in over 
three feet of snowfall and multiple day closures of roadways, businesses, and schools. The record
snowfall of January 2015 resulted from a series of storms over that month. The most recent 
significant winter event was Winter Storm Kenan (January 29, 2022), which resulted in 30.9” of 
snow in Massachusetts (Stucker, 2022).

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T able 25: Winter-Related Federal Disaster Declarations, 1978-2023 
Disaster Name Date of Event 
Coastal Storms, Flood, Ice & Snow February 1978 
Winter Coastal Storm December 1992 
Blizzard March 1993 
Blizzard January 1996 
Snowstorm March 2001 
Snowstorm February 2003 
Snowstorm December 2003 
Snowstorm January 2005 
Severe Winter Storm, Snowstorm January 2011 
Severe Winter Storm, Snowstorm, Flooding February 2013 
Severe winter storm, snowstorm, flooding January 2015 
Severe winter storm and Snowstorm March 2018 
Severe winter storm and flooding March 2018 
Severe winter storm and snowstorm January 2022 
Sources: OpenFEMA Dataset: Disaster Declarations and FEMA Declared Disasters 
Winter storms are a community-wide hazard in Winthrop. Map 6 in Appendix A illustrates the
average annual average snowfall in Winthrop, which is between 48 to 72 inches. 
The majority of blizzards and ice storms in the region cause more inconvenience than serious
property damage, injuries, or deaths. However, periodically, a storm will occur which is a true
disaster, and necessitates intense large-scale emergency response. The impacts of winter storms
are often related to the weight of snow and ice, which can cause roof collapses and also causes
tree limbs to fall. This in turn can cause property damage and potential injuries. Power outages
may also result from fallen trees and utility lines. 
A number of public safety issues can arise during snowstorms. Impassible streets are a challenge
for emergency vehicles and affect residents and employers. Large piles of snow can also block
sight lines for drivers, particularly at intersections. Refreezing of melting snow can cause
dangerous roadway conditions. In addition, transit operations may be impacted, as they were in
the 2015 blizzards which caused the closure of the MBTA system for one day and limited services
on the commuter rail for several weeks. 
Managing snow removal can be an expensive and challenging task for a community like
Winthrop. Narrow streets, lack of off-street parking options and limited areas to store plowed
snow can hinder plowing and emergency vehicle access. The Winthrop DPW works to clear roads
as requested by emergency service providers and carries on general snow removal operations.

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Probability of Future Occurrences 
Blizzards are considered high frequency events based on past occurrences, as defined by the
Resilient MA Plan. This hazard is almost certain to occur at least once a year. 
WINTER ICE STOMS 
The ice storm category covers a range of different weather phenomena that collectively involve
rain or snow being converted to ice in the lower atmosphere leading to potentially hazardous
conditions on the ground. Ice storm conditions are defined by liquid rain falling and freezing on
contact with cold objects, creating ice buildups of one-fourth of an inch or more. An ice storm
warning, which is now included in the criteria for a winter storm warning, is issued when a half inch
or more of accretion of freezing rain is expected. 
Sleet and hail are other forms of frozen precipitation. Sleet occurs when raindrops fall into
subfreezing air thick enough that the raindrops refreeze into ice before hitting the ground. The
difference between sleet and hail is that sleet is a wintertime phenomenon whereas hail falls from
convective clouds (usually thunderstorms), often during the warm spring and summer months (a
description of hail is included in a subsequent report section). Another form of freezing
precipitation is ice pellets, which occur when snowflakes melt into raindrops as they pass through a
thin layer of warmer air. The raindrops then refreeze into particles of ice when they fall into a
layer of sub-freezing air near the surface of the earth. 
The extent of ice storms is measured by the Sperry-Piltz Ice Accumulation Index (SPIA®); see
Table 23. The SPIA Index is to ice storms what the Enhanced Fujita Scale is to tornadoes, and what
the Saffir – Simpson Scale is to hurricanes. The SPIA® Index, is a forward-looking, ice accumulation
and ice damage prediction index that uses an algorithm based on three key parameters: 
1) Storm total rainfall, converted to ice accumulation 
2) Wind 
3) Temperatures during the event period 
These parameters, when used in conjunction with digital forecasts from local NWS Weather 
Forecast Offices (WFOs), have been shown to accurately predict the duration, intensity and 
damage capability of ice storms. The SPIA® Index predicts the projected footprint, total ice 
accumulation, and resulting potential damage from approaching ice storms. It is a tool to be used 
for risk management and/or winter weather preparedness Table 26). 
The best available data on previous ice storm events are recorded for Suffolk County by NOAA’s 
National Centers for Environmental Information (NCEI) Storm Events Database. Suffolk County,
which includes the Town of Winthrop, does not have any ice storms recorded since 2000. The 
Town’s location in the milder coastal region makes it less vulnerable to ice storms than adjacent
inland areas at higher elevations such as Middlesex County and central to western Massachusetts.

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Table 26: Sperry-Piltz Ice Accumulation Index (SPIA®) 
Source: SPIA® Index, www.spia-index.com/ 
Should an ice storm occur in Winthrop, the greatest hazard is created by freezing rain conditions,
which is rain that freezes on contact with hard surfaces leading to a layer of ice on roads,
walkways, trees, and other surfaces. The conditions created by freezing rain can make driving
particularly dangerous and emergency response more difficult. The weight of ice on tree branches
can also lead to falling branches causing power outages and blocking roadways. The impacts of
winter storms may also include roof collapses and property damage and injuries related to the
weight of snow and ice. 
Probability of Future Occurrence 
In Winthrop, ice storms are considered to be low frequency events based on past occurrences, as
defined by the Resilient MA Plan. This hazard may occur once in 5 years to once in 50 years, with
2% to 20% chance of occurring each year. 
Winter Weather and Climate Change 
As with hurricanes, warmer ocean water and air will provide more fuel for winter storms. 
According to the 2018 SHMCAP it appears that Atlantic coast nor’easters are increasing in

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frequency and intensity. Further, the SHMCAP notes that research suggests that warmer weather
in the Arctic is producing changes to atmospheric circulation patterns that favor the development
of winter storms in the Eastern United States. There is also some indication that as winters warm,
temperatures may be more likely to produce icing conditions. Massachuset ts’ 2022 Climate 
Change Assessment predicts more mild winters, increased precipitation in the winter months, and
multiple freeze-thaw cycles every winter due to warming temperatures . 
OTHER SEVERE WEATHER (THUNDERSTOMS / HAIL) 
THUNDERSTORMS 
While less severe than the other types of storms discussed, thunderstorms can lead to localized
damage and represent a hazard risk for communities. A thunderstorm typically features lightning,
strong winds, and rain and/or hail. Thunderstorms sometime give rise to tornados. On average,
these storms are only around 15 miles in diameter and last for about 30 minutes. A severe
thunderstorm can include winds of close to 60 mph and rain sufficient to produce flooding. The
severity of thunderstorms ranges from commonplace and of short duration to intense storms that
cause damage due to high winds, flooding, or lightning strikes. 
The extent of damages from high winds is described by the Beaufort Wind Scale (Table 27),
which was developed in 1805 by Sir Francis Beaufort of the U.K. Royal Navy. 
Table 27 Beaufort Wind Scale 
Force 
Wind
(Knots) 
WMO
Classifi- 
cation 
Appearance of Wind Effects 
On the Water On Land 
0 < 1 Calm Sea surface smooth and mirror-like Calm, smoke rises vertically 
1 1-3 Light Air Scaly ripples, no foam crests Smoke drift indicates wind direction,
still wind vanes 
2 4-6 Light Breeze 
Small wavelets, crests glassy, no
breaking 
Wind felt on face, leaves rustle, vanes
begin to move 
3 7-10 Gentle Breeze 
Large wavelets, crests begin to break,
scattered whitecaps 
Leaves and small twigs constantly
moving, light flags extended 
4 11-16 Moderate Breeze 
Small waves 1-4 ft. becoming longer,
numerous whitecaps 
Dust, leaves, and loose paper lifted,
small tree branches move 
5 17-21 Fresh Breeze 
Moderate waves 4-8 ft taking longer
form, many whitecaps, some spray Small trees in leaf begin to sway

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6 22-27 Strong Breeze 
Larger waves 8-13 ft, whitecaps
common, more spray 
Larger tree branches moving, whistling
in wires 
7 28-33 Near Gale Sea heaps up, waves 13-19 ft, white
foam streaks off breakers 
Whole trees moving, resistance felt
walking against wind 
8 34-40 Gale 
Moderately high (18-25 ft) waves of
greater length, edges of crests begin to
break into spindrift, foam blown in
streaks 
Twigs breaking off trees, generally
impedes progress 
9 41-47 Strong Gale 
High waves (23-32 ft), sea begins to roll,
dense streaks of foam, spray may
reduce visibility 
Slight structural damage occurs, slate
blows off roofs 
10 48-55 Storm 
Very high waves (29-41 ft) with
overhanging crests, sea white with
densely blown foam, heavy rolling,
lowered visibility 
Seldom experienced on land, trees
broken or uprooted, "considerable
structural damage" 
11 56-63 Violent Storm 
Exceptionally high (37-52 ft) waves,
foam patches cover sea, visibility more
reduced 
12 64+ Hurricane 
Air filled with foam, waves over 45 ft,
sea completely white with driving spray,
visibility greatly reduced 
Source: NOAA Storm Prediction Center 
In the National Risk Index, a Lightning Risk Index score and rating represent a community's
relative risk for Lightning when compared to the rest of the United States. A Lightning Expected
Annual Loss score and rating represent a community's relative level of expected building and
population loss each year due to Lightning when compared to the rest of the United States.
Winthrop is in the Low to Relatively Low categories of Lightning Risk as shown in Figure 25. 
The amount of rainfall expected for storms of various durations and recurrence intervals, from 5 
minutes to 60 days, and from annual recurrence to 1,000 years, is provided by NOAA’s Atlas 14. 
The Depth-Duration-Frequency curves are shown in Figure 26. 
For example, the chart shows the range of expected precipitation for a 12-hour rainfall ranges
from about 2 inches for annual storm and 10 inches for a storm of 100-year frequency. 
The best available data on previous occurrences of thunderstorms in Winthrop are from the
NOAA National Centers for Environmental Information (NCDC) for Suffolk County. Between the
years 2010 and 2024 NCEI records show 34 thunderstorm events in Suffolk County (Table 28).
These storms resulted in a total of $ 678,200 in property damages. There were no injuries or
deaths.

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Figure 25: National Risk Index for Lightning 
Source: FEMA National Risk Index 
Figure 26: Depth-Duration-Frequency Curve 
Source: NOAA Atlas 14

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Table 28: Suffolk County Thunderstorm Events, 2010 through 2024 
Date Max. Wind 
Speed (mph) Deaths Injuries Property 
Damage 
6/1/2010 50 0 0 10000 
6/3/2010 50 0 0 500 
6/6/2010 50 0 0 145000 
6/24/2010 50 0 0 15000 
6/1/2011 50 0 0 20000 
8/19/2011 50 0 0 15000 
6/8/2012 50 0 0 30000 
9/8/2012 50 0 0 5000 
7/3/2014 50 0 0 15000 
8/4/2015 50 0 0 50000 
2/25/2016 60 0 0 20000 
6/29/2016 50 0 0 15000 
7/18/2016 50 0 0 70000 
7/23/2016 50 0 0 83000 
6/27/2017 50 0 0 1000 
7/12/2017 50 0 0 1000 
8/2/2017 50 0 0 1000 
9/14/2017 57 0 0 25000 
7/17/2018 45 0 0 1300 
7/31/2019 65 0 0 39500 
8/7/2019 50 0 0 300 
5/15/2020 50 0 0 3500 
6/28/2020 50 0 0 1800 
7/23/2020 50 0 0 800 
10/7/2020 57 0 0 0 
6/29/2021 50 0 0 500 
6/30/2021 50 0 0 1800 
7/7/2021 55 0 0 1000 
7/27/2021 61 0 0 86900 
5/22/2022 50 0 0 11800 
8/7/2022 50 0 0 0 
7/25/2023 50 0 0 0 
7/27/2023 50 0 0 5000 
6/14/2024 50 0 0 2500 
TOTAL 0 0 $678.200 
Source: NOAA, National Centers for Environmental Information 
Magnitude refers to maximum wind speed in knots. 
Severe thunderstorms are a Town-wide hazard for Winthrop. The Town's vulnerability to severe
thunderstorms is similar to that of Nor'easters. High winds can cause falling trees and power
outages, as well as obstruction of key routes and emergency access. Heavy precipitation may
also cause localized flooding, both riverine and urban drainage related.

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Probability of Future Occurrence 
Based on the record of previous occurrences, severe thunderstorms in Winthrop are high
frequency events as defined by the Resilient MA Plan. This hazard occurs more frequently than
once in 5 years (greater than 20% per year). 
Thunderstorms and Climate Change 
As noted previously, the intensity of rainfall events has increased significantly, and those trends
are expected to continue. Neither the SHMCAP, nor the 2022 Massachusetts Climate Change
Assessment, specifically address whether climate will affect the intensity or frequency of
thunderstorms. 
HAIL 
Hail and sleet are forms of frozen precipitation. Hail occurs when precipitation falls through
subfreezing air thick enough that the raindrops freeze into ice before hitting the ground. While
sleet is a wintertime phenomenon, hail falls from convective clouds (usually thunderstorms), often
during the warm spring and summer months. 
Hail size typically refers to the diameter of the hailstones. Warnings and reports may report hail
size through comparisons with real-world objects that correspond to certain diameters, shown in
Table 29. 
Table 29: Hail Size Comparisons 
Description Diameter (inches) 
Pea 0.25 
Marble or mothball 0.50 
Penny or dime 0.75 
Nickel 0.88 
Quarter 1.00 
Half dollar 1.25 
Walnut or ping pong ball 1.50 
Golf ball 1.75 
Hen's egg 2.00 
Tennis ball 2.50 
Baseball 2.75 
Tea cup 3.00 
Grapefruit 4.00 
Softball 4.50 
Source: NOAA 
The best available local data for previous hailstorm events in Winthrop are for Suffolk County
through the National Centers for Environmental Information. Suffolk County experienced five hail

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events from 2010-2025 shown in Table 39. There were no injuries, deaths, or property damage
reported for these hail events. 
Table 30: Suffolk County Hail Events, 2010-2025 
Date Max. Wind 
Speed (mph) Deaths Injuries Property 
Damage 
5/8/2010 1 0 0 0 
6/5/2010 0.75 0 0 0 
8/19/2011 0.75 0 0 0 
8/19/2011 1 0 0 0 
6/8/2012 0.75 0 0 0 
7/18/2012 1.25 0 0 0 
7/18/2012 0.75 0 0 0 
6/17/2013 0.75 0 0 0 
8/4/2015 1.5 0 0 0 
8/4/2015 2 0 0 0 
7/23/2016 0.75 0 0 0 
6/13/2017 0.75 0 0 0 
6/28/2020 0.75 0 0 0 
8/23/2020 0.75 0 0 0 
TOTAL 0 0 0 
s for Environmental Information 
*Magnitude refers to diameter of hail stones in inches 
Hail events are a potential town-wide hazard in Winthrop however the town has not reported
any local damage associated with hail. Should a significant hail event occur, the most likely
damage would be to vehicles, both town-owned and privately owned, windows, roofs, and other
structures, as well as some utility facilities. Damage to vegetation could cause power outages, and
damage to some buildings. People outdoors directly exposed to large hail could be at risk of
injuries in a severe hail event. Should solar energy facilitates be sited in Winthrop in the future,
they could be vulnerable to the impacts of hail. 
Probability of Future Occurrences 
Based on the record of previous occurrences, hail events in Winthrop are a Medium frequency
event. This hazard may occur once in five years to once in 50 years, with a 2% to 20% chance of
occurring each year. 
WILDFIRE/BRUSHFIRE 
A brush fire is an uncontrolled fire occurring in a forested, shrub, or grassland area. In the Boston
Metro region these fires do not grow to the size of a wildfire as seen more typically in the
western U.S. There are three different classes of wildfires:

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• Surface fires are the most common type and burn along the floor of a forest, moving slowly
and killing or damaging trees; 
• Ground fires are usually started by lightning and burn on or below the forest floor; 
• Crown fires spread rapidly by wind, jumping along the tops of trees. 
Wildfire season can begin in March and usually ends in late November. The majority of wildfires
typically occur in April and May, when most vegetation is void of any appreciable moisture,
making them highly flammable. Once "green-up" takes place in late May to early June, the fire
danger usually is reduced somewhat. 
A wildfire differs greatly from other fires by its extensive size, the speed at which it can spread
out from its original source, its potential to unexpectedly change direction, and its ability to jump
gaps such as roads, rivers and fire breaks. 
The National Wildfire Coordinating Group (NWCG) classifies the severity of wildfires based on
their acreage as follows. Winthrop falls into Class B. 
• Class A - one-fourth acre or less; 
• Class B - more than one-fourth acre, but less than 10 acres; 
• Class C - 10 acres or more, but less than 100 acres; 
• Class D - 100 acres or more, but less than 300 acres; 
• Class E - 300 acres or more, but less than 1,000 acres; 
• Class F - 1,000 acres or more, but less than 5,000 acres; 
• Class G - 5,000 acres or more (NWCG, 2023). 
Wildfires can present a hazard where there is the potential for them to spread into developed or
inhabited areas, particularly residential areas where sufficient fuel materials might exist to allow
the fire to spread into homes. The Wildland Urban Interface (WUI) is the line, area, or zone where
structures and other human development meet or intermingle with undeveloped wildland or
vegetative fuels. Urban and suburban development in or near wildland vegetation poses a threat
of wildfire damages. 
Potential Wildfire Hazard Areas 
The Massachusetts State Hazard Mitigation and Climate Action Plan includes a map that depicts
statewide fire risk incorporating three risk components: fuel, wildland-urban interface, and
topography (Figure 27). The wildland-urban interface reflects communities where housing and
vegetation intermingle, and fire can spread from structures to vegetated areas. Winthrop is in an 
area designated as “no risk” of risk on this map. 
The Town of Winthrop averages less than five small grass and brush fires each year, with a loss
of less than one acre per year due to wild fires. In many years the town does not even have any
brush fires and in the years when they do, they are small and quickly contained.

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Winthrop is almost completely built out and all new development consists of the redevelopment of
existing properties, with no Wildland Urban Interface areas in the community. Outdoor burning is
allowed from January to April with a permit from the Fire Department. The Town listed no specific
areas of concern for fire-related hazards. 
F igure 27: Wildfire Risk Areas in Massachusetts 
Source: MA State Hazard Mitigation and Climate Action Plan, 2018 
Although of low severity and frequency, wildfires would be considered a potential Town-wide
hazard in Winthrop due to its small size and relatively high density of development, if a wildfire
were to occur and not be contained. 
Probability of Future Occurrence 
There are no recorded wildfire events for Suff olk County in NOAA’s NCEI database for the last 75
years. Based on a lack of past occurrences, wildfires are of very low frequency events in Winthrop,
very unlikely, with minimal examples of historical occurrences. 
Wildfires and Climate Change 
As the climate warms, drought and warmer temperatures may increase the risk of wildfire as
vegetation dries out and becomes more flammable. Increasing frequency of lightning and increasing
damage to trees from pests, can also lead to greater fire risk. The 2022 Assessment cites
anticipated forest health degradation from increasing wildfire frequency for the Eastern Inland
Region, where Millis is located.

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EARTHQUAKES 
An earthquake is the vibration, sometimes violent, of the earth's surface that follows a release of
energy in the earth's crust due to fault fracture and movement. A fault is a fracture in the earth's
crust along which two blocks of the crust have slipped with respect to each other. Faults are
divided into three main groups, depending on how they move. 
Normal faults occur in response to pulling or tension: the overlying block moves down the inclined
dip of the fault plane. Thrust (reverse) faults occur in response to squeezing or compression: the
overlying block moves up the inclined dip of the fault plane. Strike-slip (lateral) faults occur in
response to either type of stress; the blocks move horizontally along a vertical fault past one
another. Most faulting along spreading zones is normal, along subduction zones is thrust, and
along transform faults is strike-slip. 
The cause of earthquakes in eastern North America is the forces moving the tectonic plates over
the surface of the Earth. New England is located in the middle of the North American Plate. One
edge of the North American plate is along the west coast where the plate is pushing against the
Pacific Ocean plate. The eastern edge of the North American plate is at the middle of the Atlantic 
Ocean, where the plate is spreading away from the European and African plates. New England’s 
earthquakes appear to be the result of the cracking of the crustal rocks due to compression as the
North American plate is being slowly squeezed by the global plate movements. 
Damage in an earthquake stems from ground motion, surface faulting, and ground failure in which
weak or unstable soils, such as those composed primarily of saturated sand or silts, liquefy. The
effects of an earthquake are mitigated by distance and ground materials between the epicenter
and a given location. An earthquake in New England affects a much wider area than a similar 
earthquake in California due to New England’s solid bedrock geology (NESEC). 
Seismologists use a magnitude scale known as the Richter Scale to express the seismic energy
released by each earthquake. The typical effects of earthquakes in various ranges are
summarized in Table 31. 
Table 31: Richter Scale and Effects 
Richter Magnitudes Earthquake Effects 
Less than 3.5 Generally, not felt, but recorded 
3.5- 5.4 Often felt, but rarely causes damage 
Under 6.0 At most slight damage to well-designed buildings. Can cause major
damage to poorly constructed buildings over small regions. 
6.1-6.9 Can be destructive in areas up to about 100 km. across where people live. 
7.0- 7.9 Major earthquake. Can cause serious damage over larger areas. 
8 or greater Great earthquake. Can cause serious damage in areas several hundred
meters across. 
Source: Nevada Seismological Library (NSL), 2005

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According to the MA Hazard Mitigation Plan, New England experiences an average of five
earthquakes per year. From 1668 to 2007, 355 earthquakes were recorded in Massachusetts
(NESEC). Most have originated from the La Malbaie fault in Quebec or from the Cape Anne fault
located off the coast of Rockport. The region has experienced larger earthquakes, including a
magnitude 5.0 earthquake in 1727 and a 6.0 earthquake that struck in 1755 off the coast of
Cape Anne. More recently, a pair of damaging earthquakes occurred near Ossipee, NH in
1940, and a 4.0 earthquake centered in Hollis, Maine in October 2012 was felt in the Boston
area. Historical records of some of the more significant earthquakes in the region are shown in
Table 32. 
Table 32: Historic Earthquakes in Massachusetts or Surrounding Area 
Location Date Magnitude 
MA - Cape Ann 11/10/1727 5 
MA - Cape Ann 12/29/1727 NA 
MA - Cape Ann 2/10/1728 NA 
MA - Cape Ann 3/30/1729 NA 
MA - Cape Ann 12/9/1729 NA 
MA - Cape Ann 2/20/1730 NA 
MA - Cape Ann 3/9/1730 NA 
MA – Boston 6/24/1741 NA 
MA - Cape Ann 6/14/1744 4.7 
MA – Salem 7/1/1744 NA 
MA - Off Cape Ann 11/18/1755 6 
MA - Off Cape Cod 11/23/1755 NA 
MA – Boston 3/12/1761 4.6 
MA - Off Cape Cod 2/2/1766 NA 
MA – Offshore 1/2/1785 5.4 
MA - Wareham/Taunton 12/25/1800 NA 
MA – Woburn 10/5/1817 4.3 
MA - Marblehead 8/25/1846 4.3 
MA – Brewster 8/8/1847 4.2 
MA – Boxford 5/12/1880 NA 
MA – Newbury 11/7/1907 NA 
MA - Wareham 4/25/1924 NA 
MA - Cape Ann 1/7/1925 4 
MA - Nantucket 10/25/1965 NA 
MA – Boston 12/27/74 2.3 
MA - Nantucket 4/12/12 4.5 
ME – Hollis 10/17/12 4.0 
Source: Boston HIRA 
Winthrop experienced a small, 2.3 magnitude earthquake located 2 km from it on April 10,
2009. There was no data that indicated any impacts associated with this event. On October 16,

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1963 an earthquake occurred in eastern Massachusetts of magnitude 6.3 that caused a window
to crack in Winthrop. (USGS) 
One measure of earthquake extent is ground motion, which is measured as maximum peak
horizontal acceleration, expressed as a percentage of gravity (1 g). The range of peak ground
acceleration in Massachusetts is from 10g to 20g, with a 2% probability of exceedance in 50
years, as shown in Figure 28. Winthrop is in the middle part of the range for Massachusetts
making it a moderately low area of earthquake risk within the state, although the state as a
whole is considered to have a low risk of earthquakes compared to the rest of the country. 
Although New England has not experienced a damaging earthquake since 1755, seismologists
state that a serious earthquake occurrence is possible. There are five seismological faults in
Massachusetts, but there is no discernible pattern of previous earthquakes along these fault lines.
Earthquakes occur without warning and may be followed by aftershocks. Most older buildings
and infrastructure were constructed without specific earthquake resistant design features. Town
officials noted it would be useful to map the Cape Ann fault to increase public awareness of that
significant earthquakes have occurred in the North Shore area historically, that the Town could be
subject to earthquake damage and that it should be included in capital facilities planning. 
Figure 28: Massachusetts Earthquake Probability Map 
Source: 2018 SHMCAP 
Another factor related to earthquake hazards in the greater Boston area is the process of
liquefaction, which can exacerbate the damage from an earthquake. Liquefaction may occur in
areas of soft clays or filled land, which are found in the northern portion of Winthrop (Figure 29).
During an earthquake event these soils may become unstable, effectively liquefying, destabilizing
the buildings above and potentially leading to ruptured utilities, and other related impacts.

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Figure 29 - Boston Study Region Liquefaction Potential 
Source: Baise, Laurie G., Rebecca B. Higgins ; and Charles M. Brankman, Tufts University 
Earthquakes are a hazard with multiple impacts beyond the obvious building collapse. Buildings
may suffer structural damage which may or may not be readily apparent. Earthquakes can
cause major damage to roadways, making emergency response difficult. Water lines and gas
lines can break, causing flooding and fires. Another potential vulnerability is equipment within
structures. For example, a hospital may be structurally engineered to withstand an earthquake,
but if the equipment inside the building is not properly secured, the operations at the hospital
could be severely impacted during an earthquake. Earthquakes can also trigger landslides. 
Earthquakes are a potential Town-wide hazard in Winthrop. Although new construction under the
current Massachusetts Building Code will be built to higher seismic standards, there are older
structures in Winthrop that pre-date the most recent building code. Potential earthquake damages
to Winthrop have been estimated using HAZUS-MH. Total building damages, including business
interruption losses are estimated at $375 million for a 5.0 magnitude earthquake and $2.1 billion
million for a 7.0 magnitude earthquake. Other potential impacts are detailed in Table 45. In
addition, information on geologic hazards in Winthrop can be found on Map 4 in Appendix A.

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Probability of Future Occurrence 
There are several ways the probability of future occurrences of earthquakes has been estimated. 
According to the Boston College Weston Observatory, in most parts of New England there is a
one in ten chance that a potentially damaging earthquake will occur in a 50-year time period.
Earthquakes in Winthrop are a low frequency event as defined by the Resilient MA Plan. This
hazard is likely to occur at least once by the end of the century; anticipated every 100 years. 
LANDSLIDES 
According to the USGS, “The term landslide includes a wide range of ground movement, such as 
rock falls, deep failure of slopes, and shallow debris flows. Although gravity acting on an over
steepened slope is the primary reason for a landslide, there are other contributing factors.” 
Among the contributing factors are erosion by rivers or ocean waves over steepened slopes; rock
and soil slopes weakened through saturation by snowmelt or heavy rains; earthquakes create
stresses that make weak slopes fail; and excess weight from accumulation of rain or snow, and
stockpiling of rock or ore, from waste piles, or from man-made structures. 
Landslides can result from human activities that destabilize an area or can occur as a secondary
impact from another natural hazard such as flooding. In addition to structural damage to
buildings and the blockage of transportation corridors, landslides can lead to sedimentation of
water bodies. Typically, a landslide occurs when the condition of a slope changes from stable to
unstable. Natural precipitation such as heavy snow accumulation, torrential rain and run-off may
saturate soil creating instability enough to contribute to a landslide. The lack of vegetation and
root structure that stabilizes soil can destabilize hilly terrain. 
In Massachusetts, according to the SHMCAP, the most common cause of landslides are geologic
conditions combined with steep slopes and/or heavy rains. Landslides associated with heavy rains
typically occur on steep slopes with permeable soils underlain by till or bedrock. 
There is no universally accepted measure of landslide extent, but it has been represented as a
measure of destructiveness. Table 33 summarizes the estimated intensity for a range of landslides.
For a given landslide volume, fast moving rock falls have the highest intensity while slow moving
landslides have the lowest intensity. 
Table 33: Landslide Volume and Velocity 
Estimated Volume Expected Landslide Velocity 
(m 3) Fast moving landslide (Rock fall) Rapid moving landslide (Debris flow) Slow moving landslide (Slide) 
<0.001 Slight intensity 
<0.5 Medium intensity 
>0.5 High intensity 
<500 High intensity Slight intensity 
500-10,000 High intensity Medium intensity Slight intensity 
10,000 – 50,000 Very high intensity High intensity Medium intensity 
>500,000 Very high intensity High intensity 
>>500,000 Very high intensity 
A Geomorphological Approach to the Estimation of Landslide Hazards and Risks in Umbria, Central Italy , M. Cardinali et al, 2002

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The SHMCAP utilized data from the MA Department of Transportation from 1986 to 2006 to
estimate that, on average, roughly one to three known landslides have occurred each year in the
state. A slope stability map published by the MA Geological Survey and UMass-Amherst indicates
that the most significant risk of landslide is in western Massachusetts. 
The entire Town has been classified as having a low incidence risk for landslides, less than 1.5 %
of the area is involved in land sliding. (Map 4, Appendix A). The best available data on previous
incidences of landslides in Winthrop is for Suffolk County through NOAA’s National Center For 
Environmental Information. For the 75 years from 1950 to 2025, no landslides were recorded for
Suffolk County. According to the Town, no acreage in Winthrop has historically been lost to
landslides, and there is no record of any damage caused by landslides. 
Should a landslide occur in the future, the type and degree of impacts would be highly localized, 
and the Town’s vulnerabilities could include damage to structures, damage to transportation and 
other infrastructure, and localized road closures. Injuries and casualties, while possible, would be
unlikely given the low extent and impact of landslides in Winthrop. 
Potential damages would depend on how many properties were affected. Given the relatively
high assessed value of property in Winthrop, damages affecting a single residence could exceed
$500,000, and damages affecting several homes or business properties could theoretically
exceed several million dollars. However, there are no records of such landslide damages in
Winthrop. 
Probability of Future Occurrences 
Although the Resilient MA Plan classifies landslides as high likelihood events statewide, based on
past occurrences and topographic conditions in Winthrop, landslides are very low frequency
events in the town. This hazard is very unlikely to occur and there are minimal examples of
historical occurrences. 
Climate Change and Landslides 
Changes in precipitation may increase the chance of landslides, as extreme rain events could
result in more frequent saturated soils which are conducive to landslides. Drought may also
increase the likelihood of landslides if loss of vegetation decreases soil stability. 
EXTREME TEMPERATURE HAZARDS 
AVERAGE AND EXTREME TEMPERATURES 
Extreme temperatures occur when either high temperature or low temperatures relative to
average local temperatures occur. These can occur for brief periods of time and be acute, or they

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can occur over long periods of time where there is prolonged period of excessively hot or cold
weather. Winthrop has four well-defined seasons. The seasons have several defining factors, with
temperature one of the most significant. Extreme temperatures can be defined as those which are
far outside of the normal seasonal ranges for Massachusetts. The average seasonal temperatures
for Massachusetts are: Winter (Dec-Feb) Average = 31.8°F and Summer (Jun-Aug) Average =
71°F. The lowest recorded temperature was -19°F in 1934. The highest recorded temperature for
Winthrop was 104°F in 1911, and the lowest recorded temperature was -19°F in 1934. Extreme
temperatures are a town-wide hazard in Winthrop. 
EXTREME HEAT 
While a heat wave for Massachusetts is defined as three or more consecutive days above 90°F,
another measure used for identifying extreme heat events is through a Heat Advisory from the
NWS. These advisories are issued when the heat index (Figure 30) is forecast to exceed 100-
degree Fahrenheit (F) for 2 or more hours; an excessive heat advisory is issued if forecast
predicts the temperature to rise above105 degree F. 
Figure 30 Heat Index Chart 
Source: National Weather Service 
The best available data on past occurrences of extreme heat events is from NOAA’s National
Centers for Environmental Information (NCEI) for Suffolk County, which includes Winthrop. The
NCEI records indicate that since 2010, there have been six excessive heat events recorded, with
no reported death, no injuries, and no property damage (Table 34). The hottest single day 
temperature recorded in Eastern Massachusetts by the National Weather Service’s Norton/Boston 
regional office was 104 degrees (F) on July 4, 1911.

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Table 34: Suffolk County Extreme Heat Occurrences 2000 - 2025 
Date Deaths Injuries Damages 
12/17/2000 0 0 0 
5/3/2001 0 0 0 
5/4/2001 0 0 0 
5/12/2001 0 0 0 
7/22/2011 0 0 0 
7/3/2018 0 0 0 
Source: NOAA, National Centers for Environmental Information 
Extreme heat poses a potentially greater risk to the elderly, children, and people with certain
medical conditions. However, even young and healthy individuals can succumb to heat if they
participate in strenuous physical activities during hot weather. Older adults are often at elevated
risk due to a high prevalence of pre-existing and chronic conditions; in Winthrop, approximately
20.2% of the population is over age 65. People who live in older housing stock and in housing
without air conditioning have increased vulnerability to heat-related illnesses. Areas with less
shade and darker surfaces (pavement and roofs) will experience even hotter temperatures; these
surfaces absorb heat during the day and release it in the evening, keeping nighttime
temperatures warmer as well. Map 9 in Appendix A displays areas that are among the hottest
5% of land in the MAPC region based on land surface temperature derived from satellite
imagery on July 13, 2016, when the high temperature at Logan Airport was 92 ° F. There are
t hree “hot spot” areas in Winthrop, the largest in the Winthrop Center area, as shown on Map 9 . 
Hot summer days can worsen air pollution. With increased extreme heat, urban areas are likely
to experience more days that fail to meet air quality standards. Power failures are more likely to
occur during heat waves, affecting the ability of residents to remain cool. Individuals with pre-
existing conditions and those who require electric medical equipment may be at increased risk
during a power outage. Key health risks of extreme heat are summarized in Figure 31. 
Figure 31 Health Risks Associated with Extreme Heat 
Source: Killer Heat in the United States, Union of Concerned Scientists

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The 2018 SHMCAP identifies ecosystems that are expected to be particularly vulnerable to
warming temperatures. These include cold-water fisheries, vernal pools, spruce-fir forests, northern
hardwood forests (Maple, Beach, Birch), Hemlock forests, and urban forests (due to heat island
impacts). Other Impacts on natural resources include a longer growing season and northern
migration of plants and animals, including invasive species. 
Heat Waves 
While the number of 90F+ days per year is a broad indication of extreme temperatures, an
indicator that relates more directly to public health impacts is the occurrence of multiple-day heat
waves, defined at three or more consecutive days with high temperatures 90F or higher. The
summer of 2021 was an example of this, as shown in Figure 32. 
Figure 32: Summer 2021 Temperatures, Boston Area 
Source: NOAA 
The summer of 2021 was particularly hot, with four heat waves.. Two of these lasted for five
days, one lasted four days, and one lasted three days. Overall, there were 24 days 90F or
more, 17 of which occurred during the four heat waves.

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Extreme Heat and Climate Change 
The 2022 MA Climate Change Assessment includes projections of climate-driven future increases
in average temperature and in the number of extreme heat days. The assessment also highlights
the following climate impacts related to temperatures. 
The number of days per year over 90°F is projected to increase over the next several decades,
with the amount of increase depending on whether a lower or higher greenhouse gas emission
(GHG) scenario is met. By 2070 the difference between the low and high GHG emissions
scenarios could be a doubling of the annual number of 90°F days, from 47 to 90 days. By then, it
is possible that the entire summer will be marked by temperatures above 90°F (Figure 33). This
compares to the current average of 10 to 15 days per year. With changes of this magnitude,
over the course of the next several decades, the Massachusetts climate could become more similar
to areas well to the south of New England (Figure 34). 
Figure 33: Comparison of Days Above 90F for Low and High Emission Scenarios 
Source: Somerville Climate Change Vulnerability Assessment 
Probability of Future Occurrences 
Extreme heat events are classified as very high frequency events as defined by the Resilient MA
Plan. Extreme temperature events are almost certain to occur multiple times a year.

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Warmer temperatures and more frequent heat
waves are connected to impaired human health,
increased droughts, reduced agriculture yields,
species range shifts, and damaged infrastructure. 
• By 2030, the summer mean temperature 
could increase by 3.6°F from the historical 
period (1950-2013), worsening stress on 
electric transmission and utility distribution 
infrastructure. 
• By 2070, there could be 58 fewer days 
below freezing, increasing the chance of ticks 
overwintering and reducing winter recreation 
opportunities. 
• Increase in vector borne diseases and 
bacterial infections, including West Nile Virus 
and Lyme disease due to more favorable 
conditions for ticks and mosquitoes. 
• Damage to electric transmission and utility 
distribution infrastructure associated with heat 
stress 
• Damage to rails and loss of rail/transit 
service, including flooding and track buckling 
during high heat events. 
• Reduced ability to work, particularly for outdoor workers during extreme heat, as well as
commute delays due to damaged infrastructure. 
• Freshwater ecosystem degradation due to warming waters. 
• Forest health degradation from warming temperatures and increasing pest occurrence 
EXTREME COLD 
Extreme cold is relative to the normal climatic lows in a region. Temperatures that drop decidedly
below normal and wind speeds that increase can cause harmful wind-chill factors. The severity of
extreme cold temperature is typically measured using the Wind Chill Temperature Index, which is
provided by the National Weather Service (NWS). The wind chill is the apparent temperature
felt on exposed skin due to the combination of air temperature and wind speed. The index is
provided in Figure 35. A Wind Chill warning is issued when the Wind Chill Index is forecast to fall
below -25 degrees F for at least 3 hours. 
Figure 34: Temperature Scenarios 
Source: Union of Concerned Scientists (2007)

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Figure 35. Wind Chill Temperature Index and Frostbite Risk 
Source: National Weather Service 
The best available data on past occurrences of extreme cold events are from NOAA’s National
Centers for Environmental Information (NCEI) for Suffolk County, which includes the Town of
Winthrop. There were three extreme cold events recorded by NCEI since 2005 (Table 35), which
caused one deaths, no injuries, and no property damage. The coldest single day temperature 
recorded in Eastern Massachusetts by the National Weather Service’s Norton/Boston regional 
office was -18 degrees (F) on February 9, 1933. 
Table 35: Suffolk County Extreme Cold Occurrences 2005 -2025 
Date Deaths Injuries Damages 
2/3/2007 1 0 0 
2/16/2015 0 0 0 
2/14/2016 0 0 0 
Source: NOAA, National Centers for Environmental Information 
Extreme cold is a dangerous situation that can result in health emergencies for susceptible people,
such as those without shelter or who are stranded or who live in homes that are poorly insulated
or without heat. The greatest vulnerability to the Town would be a power outage during a winter
storm, which could temporarily leave many residents without heat. The elderly and people with
disabilities are often most vulnerable. In Winthrop, 20.2% of residents are 65 years old and
over, and 29.8% have a disability. 
Probability of Future Occurrences 
Extreme cold events are classified as very high frequency events as defined by the Resilient MA
Plan. Extreme temperature events are almost certain to occur multiple times a year.

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DROUGHT HAZARDS 
Drought is a temporary irregularity in precipitation and differs from aridity since the latter is
restricted to low rainfall regions and is a permanent feature of climate. Drought is a period
characterized by long durations of below normal precipitation. Drought conditions occur in
virtually all climatic zones, yet its characteristics vary significantly from one region to another,
since it is relative to the normal precipitation in that region. Drought can affect agriculture, water
supply, aquatic ecology, wildlife, and plant life. 
In Massachusetts, droughts are caused by the prevalence of dry northern continental air and a
decrease in coastal- and tropical-cyclone activity. During the 1960's, a cool drought occurred
because dry air from the north caused lower temperatures in the spring and summer of 1962-65.
The northerly winds drove frontal systems to sea along the Southeast Coast and prevented the
Northeastern States from receiving the normal sources of moisture (see Figure 36). This is
considered the drought of record in Massachusetts. 
Figure 36: Principal Sources and Pattern of Moisture Delivery to Massachusetts 
U.S. Geological Survey Water-Supply Paper 2375, National Water Summary 1988-89 
Average annual precipitation in Massachusetts is 44 inches per year, with approximately 3-to-4-
inch average amounts for each month of the year. Regional monthly precipitation ranges from
zero to 17 inches. Statewide annual precipitation ranges from 30 to 61 inches. Thus, in the driest
calendar year (1965), the statewide precipitation total of 30 inches was 68 percent of average. 
Although Massachusetts is relatively small, it has a number of distinct regions that experience
significantly different weather patterns and react differently to the amounts of precipitation they
receive. The DCR precipitation index divides the state into seven regions: Western, Central,

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Connecticut River Valley, Northeast, Southeast, Cape Cod, and Islands. Marlborough is located in
the Northeast Region. In Marlborough drought is a potential city-wide hazard. 
The Massachusetts Drought Management Plan was revised in 2019 to change the state’s 
classification of droughts by establishing four levels to characterize drought severity beyond
normal conditions: 
• Level 0-Normal Conditions (no drought) 
• Level 1-Mild Drought (formerly Advisory) 
• Level 2-Significant Drought (formerly Watch) 
• Level 3-Critical Drought (formerly Warning) 
• Level 4-Emergency Drought (formerly Emergency) 
The Massachusetts drought levels are shown in comparison to the U.S. Drought Monitor levels in
Table 36 . The two sets of drought indices are similar, but Massachusetts combines the USDM’s 
level D2 and D3 into one category, Critical Droughts. 
Table 36: US Drought Monitor Compared to MA Statewide Drought Levels 
Source: Massachusetts Drought Management Plan, 2019 
These levels are based on the conditions of natural resources and provide information on the
current status of water resources. As dry conditions can have a range of different impacts, a
number of drought indices are available to assess these impacts. Massachusetts uses a multi-index
system that takes advantage of several of these indices to determine the severity of a given
drought or extended period of dry conditions. Drought level is determined monthly based on the
number of indices which have reached a given drought level. Drought levels are declared on a
regional basis for each of seven regions in Massachusetts. County by county or watershed-specific
determinations may also be made. A determination of drought level is based on seven indices: 
1. The Standardized Precipitation Index (SPI) reflects soil moisture and precipitation. 
2. Crop Moisture Index: (CMI) reflects soil moisture conditions for agriculture. 
3. Keetch Byram Drought Index (KBDI) is designed for fire potential assessment.

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4. The Precipitation Index is a comparison of measured precipitation amounts to historic
normal precipitation. 
5. The Groundwater Level Index is based on the number of consecutive month’s groundwater 
levels are below normal (lowest 25% of period of record). 
6. The Stream flow Index is based on the number of consecutive months that stream flow
levels are below normal (lowest 25% of period of record). 
7. The Reservoir Index is based on the water levels of small, medium and large index
reservoirs across the state, relative to normal conditions for each month. 
Table 37 shows the range of values for each of the indices associated with the drought levels.
Because drought tends to be a regional natural hazard, this plan references state data as the
best available data for previous drought occurrences. 
Determinations regarding the end of a drought or reduction of a drought level focus on
precipitation and groundwater levels. These factors have the greatest long-term impact on stream
flow, water supply, reservoir levels, soil moisture, and forest fire potential. 
Table 37: Indices Values Corresponding to Drought Index Severity Levels 
Source: Massachusetts Drought Management Plan, 2019 
The drought levels provide a framework from which to take actions to assess, communicate, and
respond to drought conditions. Drought levels are used to coordinate both state agency and local
response to drought situations. Water restrictions might be appropriate at the significant drought
stage, depending on the capacity of each individual water supply system. A critical drought level
indicates a severe situation and the possibility that a drought emergency may be necessary. A
drought emergency is one in which mandatory water restrictions or use of emergency supplies is
necessary. 
Previous Occurrences 
Because drought tends to be a regional natural hazard, the best available date on previous
drought occurrences is state-wide data, summarized below. The Executive Office of Energy and

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Environment ’s Drought Management Task Force also provides information on historic drought status 
for each drought level in Massachusetts. That information is summarized below. 
Mild Drought/Advisory 2001, 2002, 2007, 2014, 2016, 2017, 2020, 2021, 2022 
Significant Drought/Watch 2002, 2016, 2017, 2020, 2021, 2022 
Critical Drought/Warning 2016, 2017, 2020, 2022 
Emergency Drought/Emergency None 
Figure 37 shows the frequency and extent of drought events in Massachusetts since the year
2001. The graphic clearly shows an increase in severe drought events in the most recent years of
this 21-year period. In just the last seven years there have been four droughts at the extreme
level in Massachusetts, in 2016, 2017. 2020, and 2022. 
Figure 37: Weeks of Extreme Drought (2001-2022) 
Source: 
A summary of Massachusetts long term historic drought events from 1879 to 2019 is shown in
Table 30. This table was prepared for the 2019 Massachusetts Drought Management Plan, so it
does not include the more recent droughts of 2020 (Level 3) and 2021(Level 2).

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Table 38 - Chronology of major droughts in Massachusetts since 1879 
Source: Massachusetts Drought Management Plan, 2019 
As shown in Figure 38, the geographic extent of droughts from 2001 to 2017 varied greatly in
different parts of the state. Winthrop experienced between 26 and 36 weeks of severe drought
between 2001 and 2017.

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Figure 38: Weeks of Extreme Drought Mapped by Region (2001-2017) 
Source: SHMCAP 2018 
Figure 39 shows the geographic extent of each of the droughts in 2016, 2020, and 2021. The
drought of 2016 was the worst one since 1985, with more than half of the state reaching the
Extreme Drought stage for several months. This was followed by another drought four years later
in 2020, which was the most severe in Southeastern Massachusetts. Finally, in the early spring of
2021 a third, milder, drought was declared. By the summer of 2021 conditions in the northeast
region improved. 
Figure 39: Recent Massachusetts Drought Events (2016-2021) 
Source: US Drought Monitor, 2016-2021

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Potential Drought Vulnerability 
The entire Town of Winthrop is potentially vulnerable to the impacts of drought. Under a severe
long-term drought, Winthrop could be vulnerable to restrictions on water supply. However, the 
Town’s water supply comes from the Massachusetts Water Resources Authority, which operates 
two large reservoirs, Quabbin and Wachusett, which have multiple years of storage available to
offset drought impacts. The system was able to meet water demands even in the drought of 
record in the 1960s. It’s possible the MWRA sys tem could be impacted by a more severe multi-
year drought, but such a drought has not occurred since records have been kept. 
Potential damages of a severe drought could include losses of landscaped areas on private
properties as well as public facilities if outdoor watering is severely restricted. Losses could also
include potential loss of business revenues if water supplies were severely restricted for a
prolonged period. As this hazard of this severity has never occurred in Winthrop, there are no
data or estimates of potential damages, but under a severe drought scenario it would be
reasonable to expect a range of potential damages up to several million dollars due to business
interruption. 
Probability of Future Occurrence 
The SHMCAP, using data collected since 1850, calculates that statewide there is a 1% chance of
being in a drought emergency in any given month. For drought warning and watch levels, the
chance is 2% and 8% respectively in any given month. See Table 391 for more information. 
Table 39: Frequency of Massachusetts Drought Levels 
Drought Level Frequency Since 1850 Probability in a Given Month 
Drought Emergency 5 occurrences 1% chance 
Drought Warning 5 occurrences 2% chance 
Drought Watch 46 occurrences 8% chance 
Source: 2018 SHMCAP 
Droughts are a medium frequency event as defined by the Resilient MA Plan, likely to occur at
least once every 50 years (two or more occurrences in the next century) 
Droughts And Climate Change 
Droughts are projected to increase in frequency and intensity in the summer and fall as weather
patterns change. Factors contributing to this include increasing evaporation as a result of warmer
weather, earlier snow melt, and more extreme weather patterns. Information from the 2022 
Massachusetts Climate Change Assessment related to drought is included in the “Climate Change
Observations and Projections” section of this report. Additionally, the 2022 Assessment highlights 
the following drought-related impacts to the Eastern Inland region where Marlborough is located:

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• Freshwater ecosystem degradation due to drought and other impacts 
• Increased contaminant concentrations in freshwater during drought conditions 
• Loss of tree cover due to drought and other impacts

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LAND USE AND DEVELOPMENT TRENDS 
WINTHROP LAND USE 
Land use mapping is available for communities statewide from Mass GIS. Map 2 in Appendix A
shows the land use map for Winthrop, and Table 40 shows the acreage and percentage of land
in 20 categories. The largest single land use category by far in Winthrop is residential, with
712.2 acres 48.9% of the Town in the high density and multifamily residential categories
combined. The next largest land use is transportation, at 19.4 acres or 13.7% of the Town, 
followed by saltwater beach at 9.2% and saltwater wetlands at 7.2%, underscoring the Town’s 
coastal location. Commercial and industrial uses have a relatively small area of 73.3 acres, or
5.0% of the total 
Table 40: Winthrop Land Use 
Land Type Acres Percent 
Forest 2.10 0.14 
Wetland 6.47 0.44 
Open Land 42.14 2.89 
Participation Recreation 43.17 2.96 
Multifamily Residential 371.95 25.53 
High Density Residential 340.25 23.35 
Saltwater Wetland 106.93 7.34 
Commercial 71.58 4.91 
Industrial 2.19 0.15 
Transportation 199.45 13.69 
Waste Disposal 2.32 0.16 
Water 7.87 0.54 
Saltwater Beach 133.70 9.18 
Golf Course 52.04 3.57 
Marina 16.90 1.16 
Urban Public 34.96 2.40 
Cemetery 15.77 1.08 
Nursery 0.27 0.02 
Forested Wetland 0.23 .016 
Brush land/Succession 6.62 0.45 
TOTAL 1,456.91 100 
Source: MA GIS Land Use Statistics 
ECONOMIC ELEMENTS 
The economy of Winthrop employed 10,132 people in 2023., the largest employment sectors
were Health Care & Social Assistance (1,299 people), Professional, Scientific, & Technical
Services (1,085 people), and Educational Services (956 people). The breakdown of employment
in 19 categories is shown in Table 41. Figure 40 shows the trends in employment over the period
2002 to 2022.

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Table 41 Winthrop Employment by Category, 2023 
Industry Workforce Percent 
Agriculture, Forestry, Fishing & Hunting 15 0.15% 
Mining, Quarrying, & Oil & Gas Extraction 9 0.09% 
Construction 524 5.17% 
Manufacturing 695 6.86% 
Wholesale Trade 256 2.53% 
Retail Trade 573 5.66% 
Transportation & Warehousing 901 8.89% 
Utilities 20 0.20% 
Information 411 4.06% 
Finance & Insurance 679 6.70% 
Real Estate & Rental & Leasing 202 1.99% 
Professional, Scientific, & Technical Services 1085 10.71% 
Administrative & Support & Waste Management 462 4.56% 
Educational Services 956 9.44% 
Health Care & Social Assistance 1299 12.82% 
Arts, Entertainment, & Recreation 357 3.52% 
Accommodation & Food Services 688 6.79% 
Other Services, Except Public Administration 437 4.31% 
Public Administration 563 5.56% 
TOTAL 10,132 
Source: U.S. Census Bureau, ACS 5-year Estimate 
Figure 40 Winthrop Employment by Category, 2023 
Source: Executive MA Office of Labor and Workforce Development,-2023

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Although primarily a residential community, the Town features several unique business areas: the
Shirley Street Business District, the Highlands District, Magee's Corner District, and the Winthrop
Center District. The Town has a modestly vibrant business community, however, in recent decades
large shopping malls in the nearby North Shore region began to impact businesses in Winthrop, In
2017 the Town undertook the Winthrop Center Business District to focus on the key center of
business in the Town. The study assesses the strengths and challenges facing local businesses, and
provides recommendations to support and revitalize the district. The plan also notes concerns for
potential flooding risks. As with the predominantly residential areas of Winthrop, a portion of the
Winthrop Center business district faces flooding risks. An area along the western side of the
district is located with the FEMA AE mapped flood zone (Figure 41). The Master Plan concludes 
that “ As a community surrounded by water, Winthrop must be particularly vigilant in adhering to
resiliency standards that address threats pose by sea level rise.” 
Figure 41 Winthrop Center Business District 
Source: Winthrop Center Business District Master Plan, 2017 
DEVELOPMENT TRENDS 
With limited land area, Winthrop is largely built out, so new growth in the Town consists of
redevelopment of existing developed sites. New developments in the MAPC region are tracked
on Mass Builds. The following developments shown in Table 42 are listed in Mass Builds as
completed since the previous Hazard Mitigation Plan in 2015.

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Table 42: Winthrop Developments Completed Since 2015 
Site# DEVELOPMENT DEVELOPMENT TYPE Res. Units STATUS 
A Temple Israel 40 unit assisted living development 40 Completed 
C 
Belle Isle Bridge Bridge repair under the MA Accelerated
Bridge Replacement program, elevated one
foot in height 
--- Completed 
D 
142 Pleasant St Conversion of former nursing home into
condominiums 16 Completed 
E Winthrop Hospital Pizzuti Development Age restricted 74 Completed 
F 
Dalrymple School
redevelopment 
Renovation of abandoned school into
affordable age restricted housing. 
27 Completed 
G 60 Hermon Street Reuse of former religious facility, 5 units 5 Completed 
H 15-17 Walden St Conversion of commercial property into
condominiums 
16 Completed 
I 413-415 Shirley St. Redevelopment for 25 residential units 25 Completed 
J 
5 Fremont Street Redevelopment of office building into
mixed-use residential and commercial.
Existing offices will remain. 
22 Completed 
K 10-26 Somerset Ave Projected 30 residential units 30 Completed 
L 20 Main St Restoration to the existing structure for a
mixed-use commercial development. --- projected 
Source: Mass Builds 
CRITCAL FACILITIES 
Critical Infrastructure in Hazard Areas 
Critical infrastructure includes three categories of facilities that are important to the Town: 
• Critical Infrastructure such as water and wastewater pumps, communications, 
• Facilities that provide utility for disaster response and evacuation such as emergency
operations centers, fire and police stations, public works facilities, 
• Facilities where additional assistance might be needed during an emergency, such as
nursing homes, elderly housing, schools, day care centers, etc..

TOWN OF WINTHROP HAZARD MITIGATION PLAN
DRAFT 2025 UPDATE 
99 
The Winthrop Hazard Mitigation Team updated the Critical Facilities inventory and map from the
previous Hazard Mitigation Plan, adding additional facilities to the list and updating existing
facilities as needed. The Team identified re are xx Critical Facilities, xx of which were newly
added sites for this plan update. These are listed in Table 43x and are shown on the maps in
Appendix A. 
Table 43 – Winthrop Critical Facilities 
MAP# FACILITY NAME ADDRESS FACILITY TYPE 
1 11 - 54 Overlook Drive 11 - 54 Overlook Drive Elder Housing 
2 Atlantis Marina 550 Pleasant St Marina 
3 Beach Fire Station 416 Shirley St. Fire Station 
4 Belle Isle Marsh Water Feature 
5 Bright Beginnings Learning Center 89 Veterans Road Child Care 
7 CVS 3 Woodside Ave. Pharmacy 
8 Cell Tower At Expert Auto 120 Shirly Street Communication Tower 
9 Cell Tower At Fellows Hall 198 Winthrop Street Communication Tower 
10 
Cell Tower At St. Johns the Evangelist
Church 320 Winthrop Street Communication Tower 
11 Cell Tower At United Methodist Church 217 Winthrop Street Communication Tower 
12 Arthur Cummings School 40 Hermon St School 
13 Children's Corner Preschool 210 Pauline St. Child Care 
14 Concrete Seawall Seal Harbor Condo Flood Protection 
15 Concrete Seawall Revere Street Flood Protection 
16 Cottage Park Yacht Club 76 Orlando Ave Marina 
17 Crystal Cove Marina 529 Shirley St Marina 
18 Deer Island Waste Water Treatment 190 Tafts Ave Waste Water Treatment 
19 E B Newton 45 Pauline Street School 
21 Fire Headquarters 40 Pauline St. Fire Station 
22 For Kids Only Extended Day in Parish School 233 Winthrop Child Care 
23 Gorman/ Fort Banks Elementary School 101 Kennedy Road School 
24 Golden Drive 1 - 22 Golden Drive Special Needs 
26 John Clark House (N Suffolk Mental Health) 152 Pleasant St Assisted Living 
27 King Gardens 2 Kennedy Road Elder Housing 
28 Lewis Lake Tidal Gate Washington Ave Flood Prevention 
29 Lodge Elks Marina 191 Washington Ave Marina 
30 Loring Rd Boat Ramp Loring Rd Boat Ramp

TOWN OF WINTHROP HAZARD MITIGATION PLAN
DRAFT 2025 UPDATE 
100 
MAP# FACILITY NAME ADDRESS FACILITY TYPE 
31 Memorial Auditorium 149 Pauline Street School 
32 Mrs. Marley's Nursery School 415 Shirley Street Child Care 
33 North Suffolk Mental Health 225 Pleasant St. Special Needs 
34 North Suffolk Mental Health 133 Morton St. Assisted Living 
35 North Suffolk Mental Health 138 Morton St. Assisted Living 
36 North Suffolk Mental Health 11 Pearl Ave Assisted Living 
37 Old Town Garage 233R Winthrop Street Kennel 
38 Pico Sewer Pump Station Pico Ave Sewer Pump Station 
39 Pier Off Court Rd Recreation 
40 Private Pier Off Court Rd Recreation 
41 Pleasant Court Sewer Pump Station Pleasant Ct Sewer Pump Station 
42 Pleasant Park Yacht Club 562 Pleasant St Marina 
43 Pleasant Times Day Care 65 Putnam St Child Care 
44 Point Shirley Association 1032 Shirley St Shelter 
45 Police Station 3 Metcalf Sq. Police Station 
46 Post Office 5 Michaels Mall Post Office 
47 Public Landing 700 Shirley St Water Access 
48 Public Safety Communication Tower Faun Bar Ave Communication Tower 
49 Recreation Center 45 Pauline St After School Program 
50 Revere St Sewer Pump Station Revere St Sewer Pump Station 
51 Rice’s Wharf 585R Shirley St Marina 
54 Skatting Rink Pauline St. Place of Assembly 
55 St John The Evangelist Church 320 Winthrop St Church 
56 St John's Episcopal Church 225 Bowdoin St Church 
57 Stone Breakwater Winthrop Shore Dr. Flood Prevention 
58 Stone Revetment Forth Heath Revetment 
59 Stone Revetment Winthrop Shore Dr. Revetment 
60 Stone Revetment Grovers Ave. Revetment 
61 Stone Revetment Winthrop Highlands Revetment 
62 Temple Tifereth Israel 93 Veteran's Rd Church 
64 Town Hall 1 Metcalf Sq. Municipal 
65 Union Congregational Church 22 Tewksbury St Church 
66 United Methodist Church 217 Winthrop St Church

TOWN OF WINTHROP HAZARD MITIGATION PLAN
DRAFT 2025 UPDATE 
101 
MAP# FACILITY NAME ADDRESS FACILITY TYPE 
67 Viking Gardens 107 Putnam St. Elder Housing 
68 Winthrop Country Day Learning Ctr. 96 Winthrop St. Child Care 
69 Winthrop DPW Building 100 Kennedy Rd. Municipal 
70 Winthrop Traffic Control Point Main St && Revere St Traffic Control Point 
70 Winthrop EOC 30 Herman St Emergency Operations Center 
71 Winthrop Traffic Control Point Shirley St & Washington Ave Traffic Control Point 
73 Yirrell Beach Off Shirley St Water Feature 
74 Winthrop Middle School 151 Pauline St School 
75 Winthrop Senior Center 35 Harvard St Senior Center 
76 Winthrop Place 26 Sturgis St Elder Housing 
77 Winthrop Middle/High School 400 Main Street School 
78 Winthrop Traffic Control Point Shirley St && Veterans Rd Traffic Control Point 
80 Winthrop Traffic Control Point Main St && Pleasant St. Traffic Control Point 
81 Winthrop Market Place 35 Revere Street Grocery Store 
82 Winthrop Traffic Control Point Revere St && Shirley St Traffic Control Point 
83 Winthrop Traffic Control Point Shore Drive && Beach Rd Traffic Control Point 
85 Winthrop Library 2 Metcalf Sq Library 
86 Winthrop Reservation Winthrop Shore Drive Water Feature 
87 Winthrop Traffic Control Point Revere St && Crest Ave Traffic Control Point 
88 Winthrop Water Storage Tank Faun Bar Ave Water Storage Tank 
89 Winthrop Yacht Club 649 Shirley St Marina 
90 Winthrop Traffic Control Point Winthrop Parkway & Revere St Traffic Control Point 
91 Private Pier off 227 Court Rd Pier 
92 Private Pier 68 Johnson Ave Pier 
93 Tafts Avenue TCP Tafts and Eliott Traffic Control Point 
94 Belle Isle Bridge Main Street Bridge 
95 Pressure Reducing Valve Station Revere Street Water Facility 
96 Power Substation Argile St Power Substation 
97 Power Substation Winthrop Street Power Substation 
Source: Winthrop Hazard Mitigation Team

TOWN OF ESSEX HAZARD MITIGATION PLAN
DRAFT 2025 UPDATE 
102 
VULNERABILITY ASSESSMENT 
The purpose of the vulnerability assessment is to estimate the extent of potential damages
from natural hazards of varying types and intensities. A vulnerability assessment and
estimation of damages was performed for hurricanes, earthquakes, and flooding. The
methodology used for hurricanes and earthquakes was the HAZUS-MH software. The
methodology for flooding was developed specifically to address the issue in many of the
communities where flooding was not solely related to location within a floodplain. 
Introduction to HAZUS-MH 
HAZUS- MH (multiple-hazards) is a computer program developed by FEMA to estimate
losses due to a variety of natural hazards. The following overview of HAZUS-MH is taken
from the FEMA website. For more information on the HAZUS-MH software, go to 
http://www.fema.gov/plan/prevent/hazus/index.shtm 
“HAZUS -MH is a nationally applicable standardized methodology and software
program that contains models for estimating potential losses from earthquakes,
floods, 

The text goes on. The rest is in the file.

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