Foreseeing Coastal
Change To Strategically
Guide Adaptation ^

CLIMATE READY

ESTUARIES

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United States
Environmental Protection
Agency

Office of Water 840R25001
January 2025


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FORESEEING COASTAL CHANGE

COASTAL EFFECTS

Change is coming to America's coasts. Sea level rise, warmer temperature, ocean
acidification, and coastal storms are further disturbing already stressed interlocking social,
economic and environmental systems. We have known for decades that storms would be
more damaging. Yet our coastal management conversations need greater awareness that
change is coming from more directions.

Most of the public discourse about coasts and resiliency focuses on storms and disasters,
walls and barriers, and resistance or retreat. However, change can derive from many paths.
Comparatively little attention goes to the staggering ecological losses of tidal wetlands.
When wetlands are discussed, the focus is usually on the hope that they protect private
property from damage. Even less public attention is paid to the stresses and impacts that
come from warming water and ocean acidification. These will compound the effects of
eutrophication, hypoxia, dead zones and harmful algal blooms that continue to resist
solutions. Sea level rise will exacerbate coastal storms but will also produce chronic impacts,
such as high tide flooding and groundwater salinization. Further, coastal change can come
from how communities gird for threats, how residents respond to their shifting personal
situations, or how the natural resource, water utility and energy sectors mitigate or exploit
new conditions.

This strategic foresight project begins a conversation about emerging risks and opportunities.
It is intended to guide coastal managers to anticipate a wider range of future conditions in
order to accelerate preparation and adaptation. It furthers the longstanding Climate Ready
Estuaries program goals of assessing vulnerabilities; developing and implementing
adaptation strategies; and engaging and educating stakeholders. The analysis and
exposition also support EPA's Office of Water priorities to improve the resilience of America's
water infrastructure; protect America's waters; advance the adaptive capacity of the
water sector; and raise the awareness of communities and decision makers.

STRATEGIC FORESIGHT

In ways that may range from unsurprising to unexpected, coastal evolution is impending
across the social, economic and environmental spectrum. Strategic foresight is a tool for
broadening awareness about what is currently out of mind yet could be just over the horizon.
This is a project to scan, identify trends, and guide coastal managers to anticipate the future.
It highlights place-based change produced by:

•	climate stressors,

•	adaptation in response to the local impacts of a changing environment, and/or

•	human action in response to global conditions.


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Although impacts will be numerous and diverse, this project focuses on topics that span
Clean Water Act intersections with coastal management. They feature developments
related to: point and nonpoint sources of pollution; healthy fish, plants, and wildlife; public
uses; and restoring and protecting habitat.

Habitat

01.	Removing tidal restrictions

02.	Resorting to floating wetlands

03.	Withstanding seagrass crashes

04.	Establishing marsh migration corridors

05.	Farming blue carbon

Infrastructure

06.	Reengineering combined sewer systems

07.	Paying for new water infrastructure

08.	Generating electricity within estuaries

09.	Truncating the tide

Water quality

10.	Providing refuge from acidification

11.	Lowering stream temperature

12.	Minding deoxygenation

13.	Enduring marine heatwaves

Society

14.	Turning to floating buildings

15.	Losing waterfront access

16.	Extending the boating season

17.	Turning to artificial intelligence

18.	Restoring abandoned sites

The scene setting stories present concepts of coastal conditions at mid-century (circa 2050).
These short narratives seed a set of two-page assessments that analyze their components
and evaluate the storylines.

METHODOLOGY

While the aim is to bring issues forward to inform policy discussions or stimulate adaptation,
at this time no one can say for certain what any place will be like in 2050. This is a look over
the horizon, which inherently entails extrapolation and some speculation. The topics were
purposely selected to bring attention to less familiar tracks and thus they may have a very
small research base. Inherently too, stories of the future describe untestable environmental
states. Inferences and judgment are required.

It is possible to craft a logical and reasonable reading of a potential future. We know that
change is being felt and stressors continue to strengthen. We see trends and movement in
the past decade such as: policy research on tidal restrictions, increasing losses of coastal
wetlands and the likelihood of even worse future losses, the accumulating tally of "billion
dollar storms," more shoreline armoring, and the rise of wind and solar power. What has been
missing from the national conversation is awareness of how developments such as these
can produce change at the scale of a place.

Information about trends, future conditions or cases related to this very diverse set of topics
can be synthesized from a range of sources such as peer reviewed literature, reports from
governments, industry, non-governmental organizations, trade journals, online maps, news
accounts, or other sources. Analysis could proceed by asking questions such as: is it already


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observed in some places? is it in experiment, planning or pilot stages? does a trend point
that way? is it an absent/present phenomenon or does it build in intensity? is it a logical
outgrowth of other policies? what do we know from analogous cases? is it contingent on
other events? how likely is this to be seen in 2050? what is the timing?

These are compact investigations to begin important conversations, they can hardly be
comprehensive. Furthermore, different people can draw different conclusions about how
U.S. coasts will be in another quarter century: crystal balls are always cloudy. This work aims
to generate thoughts about a sustainable future and support strategic planning, and
therefore the quality objectives in this project were:

1.	All report content can sustain a challenge to its reasonableness.

2.	The disseminated information is accurate, reliable, and unbiased.

3.	The assessments are useful for coastal management.

To be useful a scene setting story and its assessment must have logic, and judgment about
likelihood is justified. Decision makers cannot get a bullet-proof prediction about what the
whole U.S. shoreline will look like a quarter century from now—they can have useful
impressions which can lead to informed next steps.

Within the assessments, the stories are set out in a coastal futures section that assumes they
have already been realized at mid-century. An assessment adopts a future viewpoint in how
does it look and how did it happen sections, which crisply describe what happened since
the 2020s to bring about the mid-century condition. An assessment also includes a how likely
is it section that considers the probability of events occurring in that way.

Estimated chance

Terminology

> 9 in 10 ( > 90% )

Very likely

>2 in 3 (>67%)

Likely

~ 1 in 2 ( ~ 50% )

As likely as not



About an even chance

< 1 in 3 ( < 33% )

Unlikely

< 1 in 10 ( < 10% )

Very unlikely

To support policy making and strategic planning, a temporal return to the present period
allows consideration of selected opportunities and challenges which are additional factors
connected to a story line. Also provided are a few notable policy context and questions
that focus on associated management or technical subjects.

DECISION SUPPORT

The assessments are intended to envision plausible coastal trajectories and support decision
making for a sustainable future. Armed with foresight, now is the time to nudge the direction
or push for better outcomes. Regardless of whether a future condition is wanted or
unwanted, likely or not, agencies and managers can make choices to alter pathways.

Desirability

Probability = likely

Probability = unlikely

Wanted

How can it be made
even likelier?

What has to change to
bring this on?

Unwanted

What has to change to
keep this off?

How can it become even
less likely?

There is no single answer. There are many vectors. The U.S. shoreline varies considerably.
Different situations call for different tools. These assessments are not policy prescriptive and


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are meant to bring attention to looming topics. However, time is short for policy makers if
they want to affect trends and midcentury outcomes. The instruments many
environmental managers use to meet their mission generally include:

•	leadership: including setting the agenda, convening stakeholders, assembling
partners

•	research: to acquire knowledge, survey needs, produce metrics, test solutions

•	regulation: including rulemaking, guidance, compliance, enforcement

•	financial assistance: including loans, grants, cooperative agreements

•	technical assistance: including methods, tools, program development techniques,
training

•	education: including public advisories, information sharing, outreach

•	cleanups: such as at brownfield and Superfund sites

•	emergency response.

Twenty-five years does not leave much time to set a direction, develop the tools, implement
solutions, and produce satisfactory outcomes. If we are serious about protecting and
restoring water quality, increasing resilience: protecting public health: conserving land,
water and biodiversity: and spurring economic growth—then we must wrestle with the
subjects of these strategic foresight assessments.

FURTHER READING

Science Advisory Board. 1995. Beyond the Horizon: Using Foresight to Protect the
Environmental Future. EPA-SAB-EC-95-007. Washington, DC: U.S. Environmental Protection
Agency.

EPA. 2006. Shaping Our Environmental Future: Foresight in the Office of Research and
Development. EPA 600/R-06/150.

National Academies of Sciences, Engineering, and Medicine. 2016. Transitioning Toward
Sustainability: Advancing the Scientific Foundation: Proceedings of a Workshop.
Washington, DC: The National Academies Press.

EPA. Unpublished (2016). U.S. EPA Strategic Foresight Pilot Project: Report and Findings of the
Strategic Foresight Lookout Panel. Prepared for: Office of the Science Advisor and Office of
the Chief Financial Officer.

GAO. 2019. Overview of GAO's Enhanced Capabilities to Provide Oversight, Insight, and
Foresight: Statement of Dr. Timothy M. Persons, Chief Scientist and Managing Director,
Science, Technology Assessment, and Analytics, Testimony Before the Committee on
Science, Space, and Technology, Flouse of Representatives. GAO-20-306T.


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Sea level rise squeezes salt marshes against tidal
restrictions, threatening long-term wetlands persistence
and consequently the social, economic, habitat, and
water quality services they provide. Removing tidal
restrictions restores natural marsh processes and opens
new areas that can support salt marsh habitat.

REMOVING TIDAL RESTRICTIONS

COASTAL FUTURE
HOW DOES IT LOOK?

In some salt marshes, natural tidal flow was
restricted by transportation and water
infrastructure. Tidal restrictions prevented
inland marsh migration leading to increasing
wetland losses as sea level got higher. Once
these impediments were removed, salt
marsh ecosystems began migrating into
previously blocked spaces and are
establishing themselves faster than society
could build new marshes an acre at a time.
The opening of blocked areas to salt marsh
colonization restored habitat for fish and
birds and improved tidal flushing. II has been
a bright spot in the ongoing losses of marsh
habitat from sea level rise.

HOW DID IT HAPPEN?

Accelerated sea level rise was drowning low
elevation salt marshes. However, when
suitable conditions existed at higher elevation, the marshes could colonize those areas. Removing tidal restrictions allowed
more natural flow and enabled marsh migration into blocked areas. Many places modified their engineering procedures to
assess the severity of tidal restrictions and prioritize efforts to reconnect landscapes. Smaller projects often involved retrofits
to resize restrictions (e.g., upsizing culverts during routine road maintenance). Larger projects (e.g., dam, dike, levee
removal, or roadway elevation) needed extensive analysis and greater public outreach. Restored tidal flow often quickly
led to the reestablishment of characteristic species and water quality improvements as stream flow, sediment processes,
and vegetation returned to a more natural state. Salt marsh colonization of reconnected upstream areas allowed for the
ecosystem type to persist despite other losses to permanent inundation caused by sea level rise.



HOW LIKELY IS IT?

Sea level rise is already causing marsh loss. As coastal flooding
increasingly affects shoreline communities, there is growing
interest in using natural systems for hazard mitigation. Given
the turn to nature-based solutions, alarming trends for wetland
losses, interest from agencies, and establishment of
engineering best-practices and design standards, removing
tidal restrictions is likely. Considerations such as ecological
restoration potential, enhanced fish passage, flood risk,
infrastructure life cycles, and magnitude of benefits will affect
prioritization. Some coastal places have lower potential for
marsh migration due to local constraints or high rates of sea
level rise and subsidence. Tidal restrictions are most likely to be
removed when restrictive infrastructure (e.g., culverts, dams)
fails or otherwise requires significant maintenance, and
restoration poses limited flood risk to development.

A new bridge over a stream where culverts once blocked
passage (NOAA Fisheries).

Assessment 0 I -2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	Improving fish passage can overlap with salt marsh restoration as tidal restrictions impede both the movement of water
and fish.

•	More saline conditions in newly opened areas can lead to the displacement of valuable freshwater wetland and
upland habitat types, which will also need to migrate upward and inland to persist.

•	In some locations—without other hazard mitigation such as elevating buildings or buyouts—changed tidal flow may
increase flooding risks.

POLICY CONTEXT AND QUESTIONS

Land available for migration within coastal watersheds is limited and there can be social, economic, and environmental
conflicts. Tidal restrictions can be assessed and prioritized for upgrade or removal. In addition to guiding removal, best-
practices and standards can be updated to avoid introducing new tidal restrictions.

Removal can require a significant permitting effort and various approvals. Updating approved methods for cost-benefit
analysis to account for ecosystem-scale benefits and avoided risks will be helpful. This scenario connects to sustainability
goals for: clean water and sanitation • sustainable cities and communities • life below water • life on land.

Potential area available for wetland migration in response to sea level rise in the conterminous United States (Osland, Michael J., Bogdan
Chivoiu, Nicholas M. Enwright, Karen M. Thorne, Glenn R. Guntenspergen, James B. Grace, Leah L. Dale et al. "Migration and transformation
of coastal wetlands in response to rising seas." Science advances 8, no. 26 (2022): eabo51 74.

SELECTED REFERENCES

U.S. Environmental Protection Agency. Tidal Restriction Synthesis Review: An Analysis of U.S. Tidal Restrictions and
Opportunities for their Avoidance and Removal. EPA-842-R-20001, 2020.

Osland, Michael J., Bogdan Chivoiu, Nicholas M. Enwright, Karen M. Thorne, Glenn R. Guntenspergen, James B. Grace, Leah
L. Dale el al. "Migration and transformation of coastal wetlands in response to rising seas." Science advances 8, no. 26
(2022): eabo5174. htti3s://doi.ora/10.1126/sciadv.abo5174.

U.S. Environmental Protection Agency. An Integrated Framework for Evaluating Wetland and Stream Compensatory
Mitigation. EPA-840-B-22008, 2022.

New Hampshire Department of Environmental Services. Resilient Tidal Crossings: An Assessment and Prioritization to Address
New Hampshire's Tidal Crossing Infrgstructure for Coostgl Resilience. R-WD-19-20, 20


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Sea level rise drowns salt marshes faster than they can
grow and squeezes them against coastal development
causing habitat loss. Building and installing large scale
systems of floating wetlands can preserve some vital
ecological functions and services.

RESORTING TO FLOATING
WETLANDS

COASTAL FUTURE

HOW DOES IT LOOK?

Salt marshes were being
squeezed between rising
sea level and
development on their
landward side. As
estuarine marsh acreage
rapidly diminished, there
was a turn to large scale
systems of artificial floating
wetlands to maintain
some of the ecosystem
services that salt marshes
provided. While an
imperfect substitute for a
healthy wetland with rich
soil, the floating marshes
offered an alternative to
the looming
environmental
impoverishment that
would come from total
coastal wetland loss.

HOW DID IT HAPPEN?

By installing large scale systems of floating wetlands to counter losses from sea level rise, shoreline areas capitalized on the
ecosystem benefits that these engineered systems provide. Different places designed their wetlands for different priorities,
such as providing bird and wildlife habitat, dampening waves, improving water quality, or conserving fisheries. Using
buoyant containment, floating wetland systems let wetland plants grow hydroponically where water depth and wave
energy allowed. Installations do not rest on bottom habitat and were also located to avoid shading seagrasses. Because of
size limitations and limited lifespans of floating wetland systems, many places opted for groups of floating wetlands rather
than large singular installations.

HOW LIKELY IS IT?

Because salt marshes are one of the fastest disappearing ecosystems and they provide significant environmental benefits, it
is about an even chance that park and refuge managers and others will turn to floating wetland systems to ensure that
these benefits are not entirely lost. There is currently some experience with floating wetlands in controlled freshwater settings
for wastewater treatment and nutrient management. They have also been used in small plots, including in tidal areas, for
waterscaping. Floating wetlands are not as effective in high wave, high erosion areas because storms can damage or
dislodge thee structures and create potential hazards. The likelihood of adopting this strategy will be influenced by site
parameters and the particular environmental benefits that are wanted or achievable.

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Assessment 02-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	Floating wetlands can serve as public demonstration projects, offering opportunities to educate the public about the
ecosystem services that existing intact salt marshes provide and their value for adaptation.

•	Installations can be designed with variable heights to support multiple microhabitats and provide for native flora and
fauna.

•	Not all functions and services can be completely restored, and some (such as those coming from rich soil) may not be
replicable.

•	Containment can deteriorate and can be damaged by storms. Owners will need to plan for maintenance and
replacement. Best practices guides and design standards can be updated as experience is gained.

•	Locational decisions may need to be revisited as sea level rise and coastal change progress.

POLICY CONTEXT
AND QUESTIONS

Concerns with floating
wetlands installations
may include impacts to
aquatic resources, title
to submerged lands, or
competing uses such as
fishing and boating.

Most permitting
agencies are unfamiliar
with floating wetlands as
a replacement for some
of the functions of the
lost salt marshes.
Nationwide permits
could be considered.
This scenario connects
to sustainability goals
for: clean water and
sanitation • sustainable
cities and communities
• life below water • life
on land.

Visitors pose for pictures and explore the flora and fauna at the Floating Wetiands by Jurong Lake in
Singapore.

SELECTED REFERENCES

Cicero-Fernandez, D., Exposito-Camargo, J.A., and Pena-Fernandez, M. Efficacy of Juncus maritimus floating treatment
saltmarsh as anti-contamination barrier for saltwater aauaculture pollution control. Water Science & Technology 85, 10
(2022): 281 1-2826.

Hopkins, Julia el al. The Emerald Tutu: Floating Vegetated Canopies for Coastal Wave Attenuation. Frontiers in Built
Environment 8, (2022).

Kgrstens, Svenjg et g|. Constructed flooting wetlgnds mgde of naturgl materials as habitats in eutrophicoted coastal
lagoons in the Southern Baltic Sea. Journal of Coastal Conservation 25, 44 (2021).

Likitswat, Fg et g|. (2023). Designing Ecolooicgl Flooting Wetlgnds to Optimize Ecosystem Services for Urbon Resilience in
Tropicol Climgfes: A Review. Future Cities and Environment 9, 1 (2023): 1 -12.


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Estuary water temperatures are rising beyond the
optimum levels for Eelgrass. This keystone ecological
species is being replaced by Widgeon Grass.
Widgeon Grass is an imperfect replacement and is
prone to population crashes in years with high rainfall
and greater nonpoint source pollution.

WITHSTANDING SEAGRASS
CRASHES

COASTAL FUTURE

HOW DOES IT LOOK?

As estuary temperatures warmed up,
Eelgrass (Zostera marina) disappeared
from the southern portions of its range.
Eelgrass was an essential habitat and a
base of primary production. It stabilized
bottom sediment, improved water quality,
and had a role in mitigating acidification.
The replacing species, Widgeon Grass
(Ruppia maritima), filled most of the
ecological niche, but it had large swings
between years when the population
crashed and years with recoveries. Without
more stable Eelgrass coverage, the
frequent bust years for Widgeon Grass left
a hole at the base of estuary ecology.

HOW DID IT HAPPEN?

Seagrass had been struggling for some
time with the effects of nonpoint source
pollution, sea level rise and boating, and had seen wide losses compared to historical coverage. Rising water temperature
was one more stress on Eelgrass whose optimum temperature is between 60 and 70°F. Widgeon Grass preferred warmer
temperatures, with optimal growth occurring between 65 and 85°F, Thus, Widgeon Grass was able to move into the areas
where Eelgrass struggled.

Managers welcomed Widgeon Grass when Eelgrass could no longer thrive. Yet Widgeon Grass required more light, which
made it much more vulnerable to turbidity. Widgeon Grass abundance fluctuated from low levels in wet years to high levels
in dry years.

HOW LIKELY IS IT?

Eelgrass death and subsequent Widgeon Grass colonization have already been observed on the East Coast, and Eelgrass
death has been observed on the West Coast. Summer temperatures on both the East and West U.S. coasts are already
exceeding Eelgrass's optimum temperature range, and it is very likely that the area of warming will increase. While nutrient
load reductions from polluted runoff may be a solution to the Widgeon Grass population crashes, it is unlikely that this will be
achieved at large scales in the near term due to the diffuse nature of nonpoint source pollution. It is likely that where
Eelgrass is the primary seagrass species, if it is lost and replaced, estuary ecology will suffer when Widgeon Grass crashes.

OPPORTUNITIES AND CHALLENGES

•	Facilitating the conditions for a successful transition from declining Eelgrass to healthy Widgeon Grass could serve as a
model for managing other ecosystems facing changing environmental conditions.

•	Some areas that supported Eelgrass may be environmentally unsuitable for Widgeon Grass.

•	Southern varieties of Eelgrass that have more heat tolerance may be useful for seagrass restoration farther north.

•	Eelgrass declines may present opportunities to educate the public on the ecosystem services that seagrass provides
and their dependence on good water quality.

Assessment 03-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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POLICY CONTEXT AND QUESTIONS

Often restoration is the first step taken to address Eelgrass loss. However, recognizing its population declines as an effect of a
zonal shift may turn policymakers toward management options to promote more heat-tolerant species. Focusing on
Widgeon Grass resilience may also involve state or local regulations to reduce pollution. Controlling land-based sources and
investing in stormwater management would likely decrease eutrophication-caused turbidity and help to stabilize Widgeon
Grass populations. This scenario connects to sustainability goals for: clean water and sanitation • sustainable cities and
communities • life below water.

SELECTED REFERENCES

Plaisted, H. K., Shields, E. C., Novak, A. B., Peck, C. P., Schenck, F., Carr, J., Duffy, P. A., Evans, N. T., Fox, S. E„ Heck, S. M„
Hudson, R., Mattera, T., Moore, K. A., Neikirk, B., Parrish, D. B., Peterson, B. J., Short, F. L, & Tinoco, A. I. (2022). Influence of
Rising Wafer Temperafure on fhe Temperate Seagrass Species Eelgrass (Zostera marina L.) in the Northeast USA. Frontiers in
Marine Science, 9. https://doi.ora/10.3389/fmars.2022.920699

Plummer, M,L, Harvey, C.J., Anderson, I.E. et al. The Role of Eelgrass in Marine Community Interactions and Ecosystem
Services: Results from Ecosystem-Scale Food Web Models. Ecosystems 16, 237-251 (20131. https://doi.ora/10.1007/sl0021 -

012-9609-0

Waycott, M., Duarte, C. M., Carruthers, T. J., Orth, R. J., Dennison, W. C., Olyarnik, S., Calladine, A., Fourqurean, J. W., Heck,
K. I., Jr, Hughes, A. R., Kendrick, G. A., Kenworthy, W. J., Short, F. T., & Williams, S. L. (2009). Accelerating loss of seagrasses
across the globe threatens coastal ecosystems. Proceedings of the National Academy of Sciences of the United States of
America, 106(30), 12377-12381. https://doi.ora/l0.1073/pnas.0905620106.

Eelgrass bed (Zostera marina).

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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

The rate of sea level rise is destroying marshes. By
establishing migration corridors, these coastal
ecosystems can move upward and inland. As the tides
extend into available adjacent sites and create new
wetland conditions, salt marshes can form there while
their seaward edge is drowning.

ESTABLISHING MARSH
MIGRATION CORRIDORS

COASTAL FUTURE

HOW DOES IT LOOK?

As the rate of sea level rise exceeded
the ability of marshes to accrete
sediment, marshes were drowned and
lost. Managers searched for low lying
shoreline land that would be suitable for
new marsh habitat. In most areas, the
pace of marsh migration into available
open space was slower than the rate of
salt marsh loss due to sea level rise.

HOW DID IT HAPPEN?

In the developed areas of the country,
land that was suitable for wetlands
migration was scarce, acquisition often
involved expensive purchases. Further,
erosion control structures and impervious
surfaces hindered salt marsh migration.

A great deal of site preparation would
be required before a site was fit for
wetlands. It was very difficult to
assemble large tracts with suitable land cover, topography and hydrology.

In rural areas the best opportunities to establish salt marshes were flat, shoreline sites that had been in agricultural use.
Although assembling large tracts was still difficult, there were successes acquiring farmland that was already having trouble
with coastal flooding and salinization. Some farmers were interested in compensable conservation opportunities. States
promoted and expanded tax credits for conservation easements. Local conservation trusts formed to assist landowners with
the process of protecting their land under the easements. In other cases, programs for buyouts were expanded, and
targeted land purchases were made to ensure corridor connectivity.

Another tool, rolling easements, also became attractive as it became more widely known. These easements were triggered
by a preset amount of sea level rise, but allowed continued occupation and use until that time. This put money in farmers'
pockets right away, allowed for continued agriculture where it was viable, while securing future corridors for marsh
migration.

HOW LIKELY IS IT?

Sea level rise is already causing marsh loss. State governments, nonprofit organizations and academic groups collaborate in
many regions to model and identify land that is topographically and ecologically suitable for marsh migration. Land trusts
and other nonprofits in some coastal states along the Atlantic and Gulf are aiding with conservation easements.

Low-lying coastal cropland is widely considered an ideal setting for marsh migration, especially compared to heavily
developed urban and residential areas or coastal forests. Some coastal farming communities are already experiencing
salinization of cropland. It is very likely that shoreline farmland will become progressively more inarable in the Atlantic and
Gulf regions due to the combined effects of sea level rise, drought, and subsidence. It is likely that as tides encroach, some
rural shoreline lands will be acquired for wetlands, while it is unlikely that large corridors can be routinely assembled.

Assessment 04-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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In contrast it is unlikely that many marsh migration corridors will be established where development already exists, and large

corridors would be very unlikely. Buyout programs in residential settings are generally reactive and are most often used after

major disasters or for repetitive flood loss properties.

OPPORTUNITIES AND CHALLENGES

•	The practice of mitigation banking already considers future site conditions, including whether a site provides an
opportunity for salt marsh migration.

•	Salt marsh habitat is a direct contributor to the health of fisheries and successful marsh migration programs could have
benefits for fish.

•	Horizontal marsh migration is represented in several modeling programs, but the real-life process of salt marsh migration
is more complex than modeling is able to capture.

•	Coastal storms vary widely in strength and number from year to year and property owner interest in buyouts is likely to
increase following strong storms and fade as time goes by.

•	Remediation may be needed for land that has historically been treated with fertilizer and pesticides.

POLICY CONTEXT AND QUESTIONS

Success or failure in establishing marsh
migration corridors will hinge on how
significant economic incentives for
easements or land buyouts are and how
well they will be advertised to
landowners. Resistance to buyouts can
be expected. Private entities could be
encouraged to donate or designate
land for marsh migration through the
creation of pollution credit or tax credit
programs, or through creative market
structures that recognize the value of
ecosystem services. This scenario
connects to sustainability goals for: zero
hunger • clean water and sanitation •
life below water • life on land.

SELECTED REFERENCES

Environmental Law Institute. (2024). Compensatory Mitigation: Improving Success Under Changing Circumstances.

https://www.eli.ora/research-report/compensatory-mitiaation-improvina-success-under-chanaina-conditions

Gibson, N., McNulty, S., Miller, C„ Gavazzi, M„ Worley, E., Keesee, D., & Hollinger, D. (2021). Identification, mitigation, and
adaptation to salinization on working lands in the U.S. Southeast. Forest Service, U.S. Department of Agriculture, Southern
Research Station, https://wvvw.climatehubs.usda.aov/content/identification-mitiaation-and-adaptation-salinization-
workina-lands-us-southeast

Fant, C., Gentile, L. E„ Herold, N., Kunkle, H., Kerrick, Z., Neumann, J., & Martinich, J. (2022). Valuation of long-term coastal
wetland changes in the U.S. Ocean & coastal management, 226, 1-11. https://doi.ora/l 0.1016/i.ocecoaman.2022.106248

Stevens RA, Shull S, Carter J, Bishop E, Herold N, Riley CA, et al. (2023) Marsh migration and beyond: A scalable framework to
assess tidal wetland resilience and support strategic management. PLoS ONE 18(11): e0293177.

https://doi.ora/l 0.1371 /iournal.pone.0293177

A NRCS team surveys farmland in eastern North Carolina that is suspected to have lost
productivity due to saltwater intrusion. Photo by Michael Gavazzi/USDA.

Titus, J. (2011). Roiling Easements. U.S. Environmental Protection Agency: Climate Ready Estuaries Program. 179 pp.

https://www.epa.aov/sites/default/files/documents/rollinaeasementsprimer.pdf


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FARMING BLUE CARBON

COASTAL FUTURE

HOW DOES IT LOOK?

Natural Spartina marshes did not
capture enough annua! carbon to
become economically justifiable
carbon market projects. Entrepreneurs
with a single focus on capture and
sequestration began blue carbon
farming projects that could accumulate
carbon more efficiently than Spartina
wetlands. These designed systems did
capture more carbon, but did not
provide the same habitat complexity
and value as the native Spartina
marshes.

HOW DID IT HAPPEN?

Purposeful carbon farming could not
happen without the promise of an
economic return. Profits would only
materialize by capturing enough
carbon that could be verified. Efforts to
maximize carbon took two paths. Plants that could capture more carbon than Spartina, such as Phragmites and
mangroves were introduced. Landscape modification to improve drainage and prevent prolonged flooding was also
instituted to discourage methane production.

Phragmites captured more carbon but had different hydrology and nutrient cycling, and supported different wildlife than
native Spartina. In salt marshes that were already infested with invasive Phragmites, landowners who were after carbon
simply encouraged the Phragmites instead of working as
before to restore the natural Spartina system. Phragmites
was well-adapted to higher carbon dioxide, thus it grew
more productively and sequestered more as levels
increased. Phragmites was also well-adapted to the high
levels of nitrogen pollution in estuary waters. This made
Phragmites a low maintenance blue carbon "cash crop."

In warmer southern regions, progressively milder winters
extended the geographic range for mangroves.

Entrepreneurs speculated that assisting the northward
migration of carbon-dense mangroves would pay off if
the trees survived the winters.

Landowners altered the hydrology at their carbon farms
to minimize methane production. They also blocked the
natural migration of less carbon efficient Spartina into
their plots.

WHY THIS MATTERS

Using plants to collect carbon and sequester it in
coastal environments is a "blue carbon" contribution to
raising resilience and resisting change. Despite
ecological impacts from losing native salt marshes, a
variety of plant species could sequester carbon on
shoreline lands.

Phragmites

Assessment 05-2025
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HOW LIKELY IS IT?

Where Spartina is viable, turning to Phragmites would very likely face opposition to its intentional use for carbon
sequestration. Many local and state regulations bar planting invasive species such as Phragmites, and it is counterintuitive to
many conservationists to protect it. Further, some studies indicate that Phragmites releases more methane than Spartina,
offsetting some of the carbon benefits. Whereas translocating mangroves would replace ecologically appropriate native
wetland species, this has a better chance to be accepted by conservationists, since mangroves are native to southern U.S.
coastlines. Acceptance of assisted migration may still be unlikely because of wariness or resistance to the concept. Yet
where mangroves can survive, warmer winters are probably bringing mangroves anyway.

Markets already exist, and it is very likely that the mechanisms for accrediting blue carbon ecosystems will continue to
advance. While growing Phragmites seems like a zero-effort proposition, the costs of monitoring and accounting that are
required to participate in the marketplace are likely to outpace the revenue from credits in a modest farming operation.
Similarly, the cost of establishing a new, viable Spartina marsh would be very high compared to what it can sequester.

Unless the value of carbon becomes many fold its current price it is very unlikely that shoreline carbon farming will be a
primary activity. There is a possibility that a co-op or sponsor could relieve participating landowners of some overhead
expenses, although this too would depend on the amounts that could be credited and its price.

OPPORTUNITIES AND CHALLENGES

•	The relative ability of Spartina and Phragmites to sequester carbon still requires research, and markets need to account
for externalities such as methane.

•	Phragmites produce biomass at a faster rate than Spartina and could generate co-benefits of increased vertical
accretion and wetlands resilience to sea level rise.

•	Mangroves are moving northward, regardless of whether their migration will be assisted.

POLICY CONTEXT AND QUESTIONS

Perhaps the biggest hurdle in conserving and restoring
ecosystems through market mechanisms is actually the
creation of a robust, accessible, blue carbon market.
National accounts as well as blue carbon credits may
need to adjust when wetland vegetation changes (e.g.,
from Spartina to Phragmites or from Spartina to
mangroves). The question of regulation for intertidal
"agriculture" and uncertainty about ownership of
intertidal lands remain to be resolved. The importance of
carbon capture vs. the importance of high value native
habitat could also confront policy makers who would
want both. This scenario connects to sustainability goals
for: zero hunger • clean water and sanitation • decent
work and economic growth • responsible consumption
and production • life below water • life on land.

SELECTED REFERENCES

Emmer, I., Needelman, B., Emmett-Mattox, S., Crooks, S., Beers, L, Megonigal, P., Myers, D., Oreska, M., McGlathery, K.,
Shoch, D., (2023). Methodology for tidal wetland and seagrass restoration. Verified Carbon Standard.

https://verra.ora/methodoloaies/vm0033-methodoloav-for-tidal-wetland-and-seaarass-restoration-v2-l /

Macreadie, P.I, Costa, M.D.P., Atwood, T.B. et al. Blue carbon as a natural climate solution. Nat Rev Earth Environ 2, 826-839
(2021). https://doi.ora/10.1038/s43017-021-00224-l




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WHY THIS MATTERS

Sea level rise increases the extent and frequency of
tidal flooding, challenging shoreline municipalities that
have combined stormwater and sanitary sewer
systems. Reengineering these systems to keep tidal
floodwater out of the combined piping enables
communities to avoid harmful sewage outflows.

REENGINEERING COMBINED
SEWER SYSTEMS

COASTAL FUTURE

HOW DOES IT LOOK?

Sea level rise led to higher tides
moving inland. In low-lying
areas of coastal communities
with combined sewers, tidal
flooding eventually began
finding its way to street catch
basins and flowed down into
the pipes. Backflow preventers
kept the tide from entering the
sewer system directly through
outfalls. In contrast surface tidal
flooding entered the sewers
through catch basins that were
designed to collect runoff. Tidal
flooding overwhelmed the
pipes and produced sewage
outflows just as high rainfall did.

To stop these sewage outflows
and their ensuing problems,
communities on tidal shorelines
began reengineering their
combined sewer systems.

HOW DiD IT HAPPEN?

As tidal flooding became more frequent, strategies that worked to prevent rainfall-driven overflows, such as green
stormwater infrastructure or underground storage proved ineffective. Combined sewer systems became overwhelmed by
frequent high tide flooding events. Other available strategies included dikes or floodwalls to protect vulnerable low-lying
catch basins. In some cases, stormwater runoff became trapped behind these walls, inadvertently leading to other
drainage issues. Though expensive, some communities reconstructed their combined, single pipe systems as separate
sanitary and storm sewers to avoid having tidal inflow in their sanitary sewer systems. Those communities eliminated the
occurrence of all combined sewer overflow events because rainfall no longer entered sanitary sewers through stormwater
catch basins.

HOW LIKELY IS IT?

Combined sewer outflows cause severe negative impacts to public health, public safety, water quality, and public
finances. Because of accelerating sea level rise, coastal flooding is becoming more frequent and flooding incidents will
increase. It is very likely that coastal communities with tidal flooding problems will be forced to address their combined
systems. Communities are likely to want to use strategies that were designed to address rainfall-driven overflows because of
their familiarity; however, as time goes by the scale and frequency of tidal flooding poses challenges that these strategies
cannot address. Communities may be drawn to the additional protection from dikes or floodwalls, but the inability of
stormwater runoff to drain to open water will raise concerns. Recognizing the limitations of these alternatives, it is very likely
that exposed shoreline communities will elect to separate the vulnerable sections of their combined systems into separate
sanitary and stormwater pipes. The timing will be influenced by the onset and scale of the problem, funding, and the
availability of technical assistance.

- —

Assessment 06-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	Separating systems to avoid tidal inflow will stop combined sewer overflows, improve aquatic habitat, enhance water
quality, decrease public exposure to pathogens, and improve recreation opportunities.

•	Dikes and floodwalls will need to be reinforced intermittently to increase their stability and resistance against breaching
events as continuing sea level rise poses new flooding challenges.

POLICY CONTEXT AND QUESTIONS

Recent assessments of combined sewer system locations indicate that overflows can disproportionately affect low-income
communities and communities of color in urban areas. Policymakers will need to consider how to analyze risks, distribute the
cost burden of separating sewer systems, pay for improvements, and protect communities.

As the area subject to tidal flooding expands, more coastal communities will be challenged to meet their short-term and
long-term plans for combined sewer overflow abatement. States may struggle to meet water quality standards If outflows
increase. Policymakers may be forced to revisit compliance schedules and regulations to determine whether adjustments
are needed to address new threats. This scenario connects to sustainability goals for: good health and well-being • clean
water and sanitation • industry, innovation and infrastructure • reduced inequalities • sustainable cities and communities •
life below water • peace, justice and strong institutions.

In places with combined sewer systems, if high tide floods into the community, then water can still be draining into catch basins after the
tide level drops. This can surcharge the pipes and trigger a sewage outflow (Climate Ready Estuaries/Horsley Witten Group).

SELECTED REFERENCES

Government Accountability Office. Clean Wafer Act: EPA Should Track Control of Combined Sewer Overflows and Wafer
Quality Improvements. GAO-23-105285, 2023.

Hummel, Michelle A., Berry, Matthew S., and Stacey, Mark T. Sea level rise impacts on wastewater treatment systems along
the U.S. coast.';. Earth's Future, 6 (2018): 622-633.

Sweet, William V. et al. Global and Regional Sea Level Rise Scenarios for the United States: Updated Mean Projections and
Extreme Water Level Probabilities Along U.S. Coastlines. NOAA Technical Report NOS 01. National Oceanic and
Atmospheric Administration, National Ocean Service, (Silver Spring, MD: 2022).

U.S. Environmental Protection Agency. Report to Congress: Impacts and Control of CSOs and SSOs. EPA 833-R-04-001, 2004.


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WHY THIS MATTERS

Sea level rise and storms impair and damage water
infrastructure, necessitating reinvestment and greater
maintenance. Frequently repairing and rebuilding
these systems will increase utility costs, and long time
residents may be forced out by escalating bills or taxes.

PAYING FOR NEW WATER
INFRASTRUCTURE

COASTAL FUTURE

HOW DOES IT LOOK?

The effects of sea level rise and more
intense and frequent storms began to
have increased fiscal impacts on
coastal communities. Infrastructure
challenges came from saltwater
intrusion in drinking water sources,
higher groundwater tables, floods,
and storms. There were ever rising
costs for system maintenance, repair,
and replacement. The escalating
expense of upgrading and operating
stormwater, wastewater, and drinking
water utilities was being passed to
taxpayers and ratepayers. Some
homeowners incurred personal
expenses for their private wells or
wastewater systems. Eventually the
cost burdens began pushing long-
time residents to move away.

HOW DID IT HAPPEN?

Coastal communities faced numerous hazards and accelerating sea level rise increased their risk. Greater infrastructure
expenses were inevitable. While some needs were addressed through routine upkeep, many communities faced costly
options of elevating, hardening, and relocating facilities (many of which by function and design were located in low-lying
areas). Assets such as new drinking water sources or desalination capacity were needed to address saltwater intrusion into
aquifers and increased salinity in coastal rivers. Residents were also affected by special assessments or special service
districts, which impose levies for capital improvements. The bond market reacted to new risks by seeking higher interest,
whether the risks came from exposure to a changing environment or from borrower capacity. As costs were passed along,
some residents found the burden too high and were forced to move. For smaller water utilities, with smaller ratepayer pools
and limited capacity to access alternative funding, the dwindling number of residents and revenue only exacerbated the
situation and raised compliance challenges. Unless rate increases were paired with low-income assistance, households
faced the threat of utility shut offs. Unless new residents replaced those who moved away, those who remained faced even
higher cost burdens.

HOW LIKELY IS IT?

Coastal areas face numerous hazards and accelerating sea level rise will continue to increase the risk from floods and
storms. Vulnerable coastal communities must either adapt or be harmed by impacts, thus higher infrastructure expenses are
inevitable. Utilities that use scenarios of future conditions to inform their capital investments can raise their system resilience.
Although there are federal grant and loan programs, local governments and utilities are very likely to continue spending
their own resources on water infrastructure. Residents will shoulder many of these costs through local taxes and fees. The
availability of income-based assistance programs to buffer these impacts will very likely have geographic variability as seen
with most state and local programs. As environmental stress accumulates in coastal communities, it is very likely that
residents with limited financial means will factor all of their household expenses, including utilities, into their decisions to
remain or move away.

Assessment 07-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	Coastal infrastructure resilience can be increased through risk assessments and adaptation planning.

•	When feasible, utility resilience could also be incorporated into other necessary work such as highway maintenance or
shore protection projects.

•	People who have trouble affording rising utility bills would also have trouble paying to repair their own storm damage.

•	Underrepresentation of marginalized groups within policymaking spaces may be reinforced by out-migration, leading
to coastal communities constituted predominantly by those who can afford the rising costs of adaptation.

Construction may become a more frequent occurrence in coastal communities as
utilities increasingly need upgrades and repairs.

POLICY CONTEXT AND QUESTIONS

A focus on efficiency, water
conservation and treatment could
reduce the need for some capital
investments. Technical assistance could
raise the capacity of small systems to
manage loans and grants and to submit
competitive proposals. Restructuring or
regionalizing utilities, while not necessarily
a federal goal, has been used to
manage affordability. Federal programs
are not generally designed to assist
individuals who want to relocate
because they face rising household
expenses. While managed retreat—the
purposeful coordinated movement of
people away from risks—is intended to
retain social and community ties,
relocating due to unaffordability could
be considered as one-by-one
unmanaged retreat.

The EPA's Financial Capability Assessment Guidance (FCA Guidance) is used by municipalities when devising plans to
come into compliance with the Clean Water Act. Similarly, State Revolving Fund programs have affordability criteria based
on financial capacity and can provide very low interest rates or loan principal forgiveness. FCA and SRF examples, along
with practices of other federal programs that help with energy costs, may have wider applicability. This scenario connects
to sustainability goals for: no poverty • clean water and sanitation • industry, innovation and infrastructure • reduced
inequalities • peace, justice and strong institutions.

SELECTED REFERENCES

U.S. Environmental Protection Agency. Clean Wafer Act Financial Capability Assessment Guidance. 800b21001, 2023.

U.S. Environmental Protection Agency. Financing Decentralized Wastewater Treatment: Systems Pathways to Success with
the Clean Water State Revolving Fund Program. 832-R-22-001, 2022.

U.S. Environmental Protection Agency. Assistance That Saves: How WaterSense Partners Incorporate Water Efficiency Into
Affordability Programs. 832-F-21 -016, 2021.

Association of State Drinking Water Administrators. State Drinking Water Program Challenges and Best Practices: Small and
Disadvantaged Wgfer System Funding and Assisfgnce. 2022.

EPA's Creating Resilient Water Utilities initiative


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WHY THIS MATTERS

As the U.S. seeks to develop new energy capabilities,
the open water of coastal bays will be an enticing
place to generate electricity using wind, solar, wave or
tidal systems. Yet realizing this industrial potential will be
challenged by operational constraints, environmental
questions, and looming siting conflicts.

GENERATING ELECTRICITY
WITHIN ESTUARIES

COASTAL FUTURE

HOW DOES IT LOOK?

The push to generate electricity
for a growing population and
economy led the energy industry
to the wide-open spaces of the
country's estuaries. Environmental
conditions such as unblocked
sunlight, constant winds, and
perpetually ebbing or flooding
tides were recognized as
conducive for local energy
production to supply the coastal
towns and cities. Wind turbines,
solar arrays, wave harnessing
devices and tidal power systems
are now located on the shorelines
and throughout the open water
too.

HOW DiD IT HAPPEN?

As energy development
expanded, coastal states
developed incentives as well as
permitting and siting protocols to weigh competing uses in estuaries. Although they had less wind potential and less space
than marine sites, building estuarine facilities sidestepped some of the significant access, distance, and environmental
challenges associated with working offshore. Unshaded sunlit bays with practically 360° views to the horizon also became
home for solar electricity generation. It was inexpensive to load barges with solar panels and array and moor them in place.
In contrast, while the tides were always flooding and ebbing, tidal electricity was geographically constrained: a suitable
height range or adequate current velocity was required for economical power generation. Tidal power was practical in a
few areas, but it was not a new idea and it had already been adopted in most places where it made sense. Wave energy
in estuaries also had geographical constraints, and viability was limited to the largest most open bays. Over time
technology and battery capability advanced, such that off-the-shelf wave systems and small tidal turbines were meeting
modest needs, similar to how solar power was used for small closed systems that do not connect to the grid.

HOW LIKELY IS IT?

New energy technologies are increasingly coming online. Estuaries are attractive locations that sidestep issues of limited
space and next-door neighbors that hinder on-land energy development. Yet stakeholder conflicts have been seen with
inshore aquaculture and offshore turbines which suggest hurdles that loom for significant energy infrastructure in estuaries.
Additionally, the wind and wave potential of estuaries is small compared to marine locations.

Wind turbines are used in estuaries, often to provide power to specific facilities such as wastewater treatment plants. They
are very likely to see increased use, especially at single facilities, although the extent to which bays will be filled to
operational capacity will largely depend on area use conflicts, microeconomics, and local wind power potential. It is likely
that small self-contained wind turbines, such as those found on cruising sailboats will find greater use, especially if utility costs
rise. In contrast to wind power's reduced potential compared to adjacent marine settings, the solar energy potential of
open estuaries is probably greater than nearby terrestrial sites. The sky exposure is very high for floating arrays, and they

Assessment 08-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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don't need to take up usable space on land. Floating solar arrays have been installed in reservoirs, but their use in coastal
waters is more problematic due to salt and salt spray, as well as tidal currents and height changes. Further, waves and storm
surge introduce maintenance challenges. Smaller floating arrays, perhaps moored at piers, are likely, as they are more
practical for more locations and applications. Large area installations may face use conflicts with fishing, recreation, and
navigation. Additionally, systems may also need to be offline or protectively removed for a window of time before and after
severe weather. Floating solar power systems that take up a significant portion of a bay are unlikely. Tidal power from
impoundments or tidal currents is not new and has largely been evaluated. Much of the country's estuaries are microtidal
and probably unsuitable. Tidal power is very unlikely to become an important source of electricity in new places. If the
equipment cost is comparable to solar, then small scale, single user, shoreline wave systems could be used near the water,
in special cases such as to power equipment or lights.

OPPORTUNITIES AND CHALLENGES

•	The need for a skilled workforce to build
and maintain open-water energy
technologies and to develop supporting
infrastructure and supply chains could
support job development in coastal
communities where construction and
maintenance activities would be based.

•	The addition of commercial-scale
projects could improve the reliability and
resilience of the local grid system.

•	The environmental impacts of large
installations in bays, including shaded
bottoms or effects on fish, marine
mammals and birds will need
assessment.

•	Long-term coastal evolution from sea
level rise, coastal storms, or population
movement can change the operational
considerations for power generation.

POLICY CONTEXT AND QUESTIONS

As seen with all energy sources, favorable government incentives influence industry investments. Increasing pressure to
satisfy public demand may produce proposals for siting in the open space of coastal bays. Most of those spaces are
publicly owned. Concerns with estuary energy generation include impacts to water quality, ecological impacts, rights to
submerged lands, and competing uses such as fishing and boating. Environmental impacts could be large and increase as
installations get bigger or more prominent.

As with any energy project, there are complex siting and permitting challenges, and a multifaceted system of federal, state,
and local rules and regulations. This scenario connects to sustainability goals for: affordable and clean energy • decent
work and economic growth • industry, innova tion and infrastructure • sustainable cities and communities • life below water.

SELECTED REFERENCES

DOE. (2019). Powering the Blue Economy: Exploring Opportunities for Marine Renewable Energy in Maritime Markets. Office
of Energy Efficiency gnd Renewgble Energy.

Kircher, L., Fogorty, M., gnd Lgwson, M. (2021). Morine Energy in the United Stgtes: An Overview of Opportunities. Notionol
Renewgble Energy Lgborotory. NREL/TP-5700-78773.

Johnson Controls and GRID work with volunteers assembling and installing a
floating PV array on a Walden water retention pond at the City's water facility in
Walden, CO (U.S. Department of Energy).

Pologye, B., Vgn Cleve, B., Copping, A., grid Kirkendgll, K. (2011). Environmentol effects of tidol energy development. U.S.
Depgrtment of Commerce, NOAA Technicol Memo. F/SPO-116.


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WHY THIS MATTERS

Sea level rise and storms are leading communities to
gates that close off an estuary from the sea to reduce
their risks from flooding. Barriers must close in advance
of floods and those levels are reached more often due
to sea level rise. By truncating the tidal cycle, gate
closures change hydrology and ecological systems

TRUNCATING THE TIDE

COASTAL FUTURE
HOW DOES IT LOOK?

When cities turned to surge barriers as their
preferred way of protecting against coastal
storms and sea level rise, they saw no further
need for duplicative on-land hazard
mitigation measures. Consequently, as sea
level rise progressed, the gates were closed
more and more frequently to prevent flooding.
This operating procedure produced a
truncated tidal cycle in estuaries, with
reduced tidal range, and produced long
periods of still water when the gates were shut.

HOW DID IT HAPPEN?

Surge barriers were constructed across inlets
and river mouths. While barrier design varied
by location, all incorporated movable gates
that closed to protect areas behind the barrier
from storm surge and tidal flooding. Most
barrier designs included closed spans that
reduced the distance across the estuary mouth and constricted tidal flow to narrower openings. Gates did not close
quickly; thus closures needed to begin long before high tide. Gates remained closed until water levels equalized on both
sides of the barrier, a process that sometimes spanned a few days for strong storms. As sea level rise progressed, surge
barriers closed more frequently in response to routine tides that began to cause flooding at levels that used to only be seen
during storms.

When open, locally increased tidal velocities were seen at the barrier gates—which posed challenges to navigation.

Closing the gates reduced tidal amplitude, altered tidal mixing and salinity, introduced stratification, and affected
sediment transport within the estuary. In some instances, while surge barriers successfully protected development from
ocean storm surge, concurrent rain and high river levels led to flooding behind the closed gates.

HOW LIKELY IS IT?

It is very likely that coastal hazard risk and severity will increase in response to sea level rise and changes in extreme weather
patterns, necessitating mitigation strategies. Already, some existing surge barriers are being closed more frequently rather
than just for the extreme storms they were originally designed to protect against. Several U.S. coastal regions are
considering surge barriers as an integral element of resilience and adaptation planning. Surge barriers are included in the
tentatively selected plans in recent coastal risk management studies, including for the New Jersey Back Bays, New York-
New Jersey Harbor and Tributaries, and coastal Texas regions, though they are paired with other coastal hard infrastructure
and nature-based solutions.

It is very likely that surge barriers will lead to both acute and chronic impacts to estuaries, though the exact nature of
impacts is influenced by surge barrier design (e.g., barrier and gated opening lengths), estuary characteristics (e.g.,
stratification type, sedimentary transport, hydrodynamics), frequency and duration of gate closures, and climatic conditions
(e.g., drought). Scientific research and modeling on a limited selection of extant and proposed barriers demonstrate
impacts to tidal flow, exchange, mixing, and velocities, with cascading effects to other estuary conditions such as tidal
amplitude.

Assessment 09-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	There is a continued need for research on the chemical, physical and biological effects of surge barriers and their
operation—for the decades (and centuries) that they will be in place,

•	While existing barriers may serve as case studies, few of these barriers are of the scale being considered for
implementation in U.S. coastal cities.

•	Frequent openings and closures may reduce the operational lifespans of these structures.

•	On-land flood mitigation may still be needed for protection against smaller flood events or induced flooding.

•	As surge barriers close more frequently, and possibly for longer durations, coastal cities may find that interrupted tidal
processes and trapped pollutants behind the barrier contribute to water quality impairments and habitat degradation.

POLICY CONTEXT AND QUESTIONS

Sea level rise and changes in extreme weather patterns will continue to force U.S. coastal cities to confront how much
flooding is acceptable. Over time, barrier managers will need to consider adjustments to the water level closure criteria to
limit increasingly frequent and long closures: cities will need a greater tolerance for flooding or must adopt other mitigation
measures.

For some communities, surge barrier proposals can raise questions about which populations, infrastructure, and
neighborhoods are protected and which ones are not protected (or even which will face increased potential for harm via
induced flooding). Cities may also see increased development behind surge barriers in locations that some will believe are
safe from coastal storms and flooding. This scenario connects to sustainability goals for: sustainable cities and communities •
life below water.

SELECTED REFERENCES

Chen, Z., & Orton, P. M. (2023). Effects of storm surge barrier closures on estuary saltwater intrusion and stratification. Water
Resources Research, 59, e2022WR032317. https://doi.ora/10. l029/2022WR032317

Orton, P., Ralston, D., van Prooijen, B., Secor, D., Ganju, N., Chen, I., et al. (2023). Increased utilization of storm surge barriers:
A research agenda on estuary impacts. Earth's Future, 11, e2022EF002991. https://doi.ora/l 0.1029/2022EF002991

Ralston, D. K. (2022). Impacts of storm surge barriers on drag, mixing, and exchange flow in a partially mixed estuary. Journal
of Geophysical Research: Oceans, 127, e2021 JC018246. https://doi.ora/l 0.1029/2021JC018246

MULTIPLE LINES OF DEFENSE ON THE TEXAS COAST

Galveston Seawall
Improvements

Illustration is representational and not to scale

Bolivar and West
Galveston Beach
and Dune System

Bolivar Roads
Gate System

Concept for gates and other coastal storm risk management measures at Galveston Bay. Image from the Coastal Texas Study, Story Map
Homepage fhttps://coastal-texas-hub-usace-swa.hub.arcais.com/ downloaded Oct. 24, 2024).


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WHY THIS MATTERS

Ocean and coastal acidification can harm marine life:
especially calcifying species like shellfish. Managing
refuge areas in estuarine waters could allow for some
aquatic habitats and populations to persist.

PROVIDING REFUGE FROM
ACIDIFICATION

COASTAL FUTURE

HOW DOES IT LOOK?

Ocean acidification, which was
exacerbated by additional natural
and anthropogenic factors (e.g.,
storm and seasonal upwelling,
freshwater mixing, nutrient runoff,
phytoplankton and algal blooms),
turned once rich estuarine habitats
into stressful places for aquatic life.

Calcifying organisms were particularly
affected as waters became more
acidic and carbonate ion
concentrations decreased. In an
effort to preserve foundational
species such as clams and oysters,
water chemistry was managed in
small parts of estuaries to create
acidification refuges.

HOW DID IT HAPPEN?

Attempts to directly manipulate
acidification in estuaries took two
forms. In the first, macroalgae and seagrasses were deployed to augment local photosynthesis and thereby alter the
immediately surrounding water chemistry. In the second, calcium carbonate such as from recycled clam and oyster shells
was added to bay sediments. Other management measures addressed nonpoint source nutrient pollution that
exacerbated acidification. This had a further benefit of improving conditions for submerged aquatic vegetation. The
aquaculture industry also actively managed oysters through sensitive life cycle stages. Water chemistry monitoring allowed
the industry to handle pH and chemical variability caused by natural upwelling and other factors. Other industry strategies
included selective breeding for acidification-resistant broodstock and increasing production levels to account for mortality.

HOW LIKELY IS IT?

It will not be possible for local management of estuaries to reverse marine trends. Yet estuary management can have some
impact on local water chemistry. Because coastal and estuarine waters are particularly susceptible, and threats to some
aquatic species have significant economic implications, state and federal agencies have developed research priorities
and management strategies for ocean and coastal acidification and it is very likely that this will continue.

Directly introducing carbonate with recycled oyster shells has been tested in experimental plots. This has some potential to
change sediment carbonate levels where they are placed, although effects diminish over time. It is about an even chance
that with active and ongoing replenishment, sedimentary carbonate could be boosted with shell hash. The effectiveness of
submerged aquatic vegetation in controlling pi I is highly variable and transient. While otherwise SAV has an important
ecological role, it is unlikely to be an effective management strategy for the problem of acidification. The effects of
nonpoint sources of pollution become even more problematic as water temperatures increase, and their further
interactions with ocean acidification will become apparent. Increased control of nonpoint source pollution will be
necessary to reduce its contribution to acidification. Nutrient management with seaweed is an emerging area of interest
that is likely to be pursued for that reason, and this will have some co-benefits for addressing coastal acidification.

Assessment 1 0-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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The oyster aquaculture industry is already actively
managing operations to reduce the effects of
acidification. Water intake monitoring, pl-l
management, and bioengineeririg were seen in the
2010s and are very likely to continue and be more
widely adopted. Some industry relocation has
occurred and is as likely as not to continue, largely
dependent on the place-based effects of
acidification and the ability to mitigate its impacts.

OPPORTUNITIES AND CHALLENGES

Previous episodes of acidification mortality in the
shellfish industry have spurred the development
of partnerships with industry, agencies, and
academia.

The stress from the increasing acidification of the
ocean and the tidal mixing of seawater into
estuaries will never be eliminated, and is
projected to grow worse in coming decades.
Within larger estuaries where water chemistry
has persistent spatial variability, affected uses
might be relocatable to more favorable zones if
suitable sites are available.

Pteropod affected by ocean acidification. Its shell ridges are dissolving,
and shell fractures, weak spots, and cloudy areas are also visible (NOAA
News April 30, 2014).

POLICY CONTEXT AND QUESTIONS

Water use conflicts are not uncommon with aquaculture operations, and expansions of macroalgae aquaculture may
encounter these tensions. State and federal agencies are producing strategic research and response plans to ocean
acidification that provide a blueprint for experimentation and adaptation responses.

Nonpoint source pollution has been difficult to control without explicit legislative authorization, yet it is a critical element in
responding to coastal acidification. The question of impairments due to acidification are expected to increasingly occur
and arise in listing decisions under Clean Water Act 303(d) and TMDLs. This scenario connects to sustainability goals for:
clean water and sanitation • sustainable cities and communities • life below water.

SELECTED REFERENCES

National Oceanic and Atmospheric Administration. Ocean, Coastal, and Great Lakes Acidification Research Plan: 2020-
2029, edited by Jewett, Elizabeth B., Emily B. Osborne, Krisa M. Arzayus, Keriric Osgood, Benjamin J. DeAngelo and Jennifer
M. Minfz. 2020.

California Ocean Science Trust. Emerging understanding of the potential role otseaarass and kelp as an ocean
acidification management tool in California. Nielsen, Karina J., John J. Stachowicz, Katharyn Boyer, Matthew Bracken,
Francis Chan, Francisco Chavez, Kevin Hovel, Kerry Nickolks, Jennifer Ruesink, and Joe Tyburczy. Oakland, California. 2018.

Washington Marine Resources Advisory Council. 2017 Addendum to Ocean Acidification: From Knowledge to Action,
Washington State's Strategic Response, edited by Enviroissues. Seattle, Washington. 2017.

California Ocean Science Trust. The West Coast Ocean Acidification and Hypoxia Science Panel: Major Findings,
Recommendations, and Actions, by Chan, Francis, Alexandria Boehm, Jack Barth, Elizabeth Chornesky, Andrew Dickson,
Richard Feely, Burke Hales et al. Oakland, California. 2016.


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CLIMATE READY

S T U A R I E S

xvEPA

LOWERING STREAM
TEMPERATURE

COASTAL FUTURE

HOW DOES IT LOOK?

Streams, lakes, and estuaries
got progressively hotter as time
went on. A variety of cold-
water fish such as salmon and
trout saw their range shrink to a
few refuge areas. Some went
extinct as the last of their
habitat became too hot. Many
of these fish were iconic or
culturally significant.

In an attempt to save what
could be saved, there was a
concerted effort to control
stream temperature. Any
technique to lower water
temperature in a pond or a first-
order stream was implemented.

These measures were
expensive, and people
debated their value and long-
term effectiveness.

HOW DiD IT HAPPEN?

Traditional techniques for lowering water temperature were implemented first. Combinations of in-steam measures (e.g.,
removing obsolete dams and impoundments, creating deep pools or artificial logjams), groundwater measures (e.g.,
promoting stormwater infiltration, removing channelization) and land use measures (e.g., planting trees, restoring upland
riparian areas) to reduce water temperatures had varying impacts. As warming continued more radical steps were tried.
Reflective material was used to cover reservoirs and ponds. Some places opted for cooling towers such as those used to
lower the temperature of industrial discharges. Refrigeration was pursued to preserve endangered species on the most
critical stream reaches. On the hottest days some environmental managers tried to directly lower water temperature by
dumping ice.

HOW LIKELY IS IT?

Because many of the land use and hydrological measures used to control water temperature have multiple benefits for
other environmental management goals it is likely that they will be used if temperatures approach critical levels. However,
some of these techniques, such as tree planting, are not quick solutions and cannot be effective on short time scales.
Reflective material and blankets have been used to keep the sun off of glaciers to stop melting, and drinking water
reservoirs and aqueducts have been covered with floating covers and "shade balls" to reduce evaporation or control
algae. It is about an even chance that where feasible these techniques could be used to limit solar heating in aquatic
habitats on the hottest days. Chilling and evaporation have been used to mitigate point sources of thermal pollution, and
dumping ice might be used to lower water temperature in small impoundments or headwaters by 1 ° or 2°—however for
general environmental management these are speculative ideas with no known examples. Although it would only be
needed to keep temperature below ecological thresholds on the hottest days, chilling would be a desperate measure and
very unlikely to be widely used due to logistics, cost, uncertainty, and perception that it would be just a short-term patch.

WHY THIS MATTERS

The temperature in streams and waterbodies continues
to warm, creating major threats to sensitive fish and
aquatic life. Adopting targeted and intensive
interventions could be a last effort to lower tributary
temperatures and maintain critical habitat for
important species.

Assessment 1 1 -2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	Adopting these techniques may lead to co-benefits such as restored natural hydrology, improved water quality, and
the creation of new habitat for aquatic flora and fauna.

•	Locational decisions and best management practices may need to be updated regularly as temperatures continue to
rise.

•	Existing development may hinder the adoption of temperature reducing measures such as the removal of obsolete
dams and impoundments or the removal of channelization because these strategies could impact flooding.

•	Techniques that can lead to some water temperature reduction may fail to provide enough after further warming.
Efforts to lower stream temperature may not be sufficient and durable, they may simply delay the inevitable.

POLICY CONTEXT AND QUESTIONS

Some measures to lower stream temperature are not quick fixes and it may be too late to use them if temperature
thresholds are approaching. Advanced planning, significant engineering analysis, and time for permits and construction
need to be factored in. Some of the simpler and easier concepts, such as planting trees, can take years before there is
adequate shading.

Higher water temperature may challenge states with water quality standards related to heat. Policymakers may be forced
to revisit regulatory approaches to determine whether adjustments are needed. This scenario connects to sustainability
goals for: clean water and sanitation • sustainable cities and communities • life below water • life on land.

SELECTED REFERENCES

Batiuk, Rich el al. Rising
Watershed and Bay Water
Temperatures: Ecological
Implications and Management
Responses - A STAC Workshop.
STAC Publication Number 23-

001.	January 20, 2023.

Oregon Department of Fish and
Wildlife. The Oregon
Conservation Strategy: Climate
Change and Oregon's Estuaries.
n.d.

Thompson, Jonathan. Keeping it
cool: unraveling the influences
on stream temperature. Science
Findings 73, (2005).

U.S. Environmentoi Protection
Agency. Actions That Could
Reduce Woter Temperature,
Appendix F. Being Prepared for
Climate Change: A Workbook
for Developing Risk-Based
Adaptation Plans. EPA 842-K-14-

002,	2014.

Newly-planted vegetation along the Shasta River. Monitoring of the project has shown a
significant decrease in summer water temperatures. Erika Nortemann/NOAA


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CLIMATE READY

S T U A R I E S

xvEPA

MINDING DEOXYGENATION

COASTAL FUTURE
HOW DOES IT LOOK?

Warmer ocean water temperature directly
reduced the physical capacity of seawater
to hold dissolved oxygen. Many estuarine
and coastal waters already had unique
hypoxia problems resulting from land-based
sources of pollution and other human
activity. While nutrient driven hypoxia in
coastal waters continued to resist solutions,
reduced oxygen capacity due to warming
made estuary recovery more difficult and
pushed marginal places into hypoxic states.

HOW DID IT HAPPEN?

The main mechanisms through which
warming water temperature contributed to
oxygen stress in coastal waters was by
lowering the physical ability to hold dissolved
oxygen and by induced stratification that
isolated bottom water. Sea level rise
increased estuarine salinity which also led to lower oxygen solubility.

As temperatures rose, estuaries entered hypoxic states when oxygen was depleted. More waters showed signs of hypoxia
and became more sensitive to the negative water quality impacts of nutrient loading. As warming continued, coastal and
estuarine areas were being added instead of removed from impaired waters lists.

HOW LIKELY IS ST?

In marine waters, 0.5-3.3% of dissolved oxygen was
lost from the upper 1000 m between 1970 and
2010. Half of this decline is attributed to solubility
reduction, and the balance to stratification,
circulation and other factors. The mechanisms for
deoxygenation in estuaries are similar: the
questions are about the likelihood and the
magnitude of the impact.

It is very unlikely that an estuary with good water
quality will become hypoxic due solely to the lower
dissolved oxygen capacity of warmer water.
Marine water at 100°F can still hold 5.5 mg/l of
dissolved oxygen.

The main path by which warming can impact
oxygen levels seems to be through stratification.
Where stratification exists it is about an even
chance that it will strengthen, and elsewhere

Assessment 1 2-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001

WHY THIS MATTERS

Warmer temperature lowers the capacity of water to
hold dissolved oxygen, and increases the potential for
stratification which can lead to lower bottom oxygen
levels. Warmer water can intensify the hypoxia already
seen in so many U.S. estuaries, and can tip other places
into this impaired condition.

Dissolved oxygen solubility (mg/l at 760 mm Hgj

Salinity

40°F

50°F

60°F

70°F

80°F

90°F

100°F

0

12.96

11.29

9.96

8.90

8.02

7.28

6.64

5

12.53

10.93

9.66

8.64

7.79

7.08

6.47

10

12.12

10.59

9.37

8.39

7.58

6.89

6.30

15

11.72

10.26

9.09

8.15

7.37

6.71

6.14

20

11.33

9.93

8.82

7.91

7.16

6.53

5.98

25

10.95

9.62

8.55

7.69

6.97

6.36

5.83

30

10.59

9.32

8.30

7.46

6.77

6.19

5.68

35

10.24

9.02

8.05

7.25

6.58

6.02

5.53

Source: Dissolved oxygen solubility tables https://water.usas.aov/water-
resources/software/DOTABLES/


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when hydrology is conducive to stratification it can emerge. Whether new or intensified stratification will have the strength
or duration to produce hypoxia depends on the unique circumstances of every place. Areas that already have low oxygen
would be the most susceptible.

OPPORTUNITIES AND CHALLENGES

•	Reductions in eutrophication-induced hypoxia could outweigh any increases in hypoxia due to change in temperature.

•	Hypoxic conditions can drive finfish to swim away from impacted areas and can have lethal effects for stationary
organisms.

POLICY CONTEXT AND QUESTIONS

A great number of U.S. estuaries experience hypoxic conditions. Water temperature increases are an additional stressor.
More estuaries that are currently marginal can be expected to start having hypoxic events. Consideration of greater
controls for point and nonpoirit source pollution may be due. This scenario connects to sustainabiiity goals for: clean water
and sanitation • sustainable cities and communities • life below water.

Change in number of U.S. coastal areas experiencing hypoxia from 12 documented areas in 1960 to over 300 in 2008. Coastal Areas
Experiencing Hypoxia (Committee on Environment and Natural Resources. 2010. Scientific Assessment of Hypoxia in U.S. Coastal Waters.
Interagency Working Group on Harmful Algal Blooms, Hypoxia, and Human Health of the Joint Subcommittee on Ocean Science and
Technology, https://cfpub.epa.aov/si/si public record report.cfm?Lab=NHEERL&dirEntrvld=213608 )

SELECTED REFERENCES

K.E., Hinson, M.A.M., Freidrichs, R.G., Najjar, M.. Herrmann, 7.., Bian, G„ Bhatt, P., St lauienl, II., Tian, G., Shenk. (2023).
Impacts and uncertainties of climate-induced changes in watershed input on estuarine hypoxia. European Geosciences
Union, https://www.usas.aov/publications/impacts-and-uncertainties-climate-induced-chanaes-watershed-inputs-
estuarine-hvpoxia

Changing Ocean, Marine Ecosystems, and Dependent Communities. Special Report on the Ocean and Cryosphere in a
Changing Climate, https://doi.ora/10.1017/9781009157964.007.

Sixth Assessment Report, Working Group 1: The Physical Science Basis. Chapter 5: Global Carbon and other Biogeochemical
Cycles and Feedbacks. 5.3.3.2 Ocean Deoxygenation and its Implications for Greenhouse Gases

https://www.ipcc.ch/report/ar6/wa1 /chapfer/chapter-5/#5.3%20%205.3.3.2


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Marine areas have become prone to heatwaves of
several days when water temperature is very high. As
unusually warm seawater flows into estuaries their
temperature rises too. These events have had notable
social, economic and environmental impacts that offer
a glimpse of the future and the need for adaptation.

ENDURING MARINE HEATWAVES



T"

, MfcO-"-15,. ,

iBP^P liLH

	M ...iMAIto



to
<5=3

J J hh a, A MlJ

—

COASTAL FUTURE

HOW DOES IT LOOK?

Warming ocean temperatures and
marine heatwaves (periods of persistent
anomalously warm ocean
temperatures) diffused into estuaries
with notable effects. Heatwaves
became increasingly frequent and
were an obstacle to clean water
management goals. While managers
could do little to influence coastal
water temperature, heatwaves
provided previews of effects to come
when warmer water would be the
norm.

HOW DID IT HAPPEN?

Ocean temperatures were naturally
variable in response to regional-scale
heat transfer, warming processes and
the influence of broader climate
modes. However, oceans did continue
to generally accumulate heat and marine heatwaves occurred more frequently. U.S. coasts experienced heatwaves of
varying intensity and duration and the warm ocean water was brought into estuaries by tides.

In estuaries heat was associated with algae blooms, bacteria, stress on immobile organisms including submerged aquatic
vegetation, exacerbation of low oxygen states, and temporary biological shifts—both in and out. While of limited duration,
heatwaves were harbingers of future conditions. Temperature-sensitive and immobile marine organisms, as well as those at
the warm (usually southern) edge of their distribution range, were the most vulnerable to excess heat. Coastal ecosystems
shifted as heat stress overwhelmed cool-water kelp, seagrass, and coral habitats. The resulting habitat conversions and
effects from food web alterations led to disruptions in the fishing, aquaculture, and tourism industries.

HOW LIKELY IS IT?

In 2013-2016 the Northeast Pacific Ocean "Blob" produced: seabird and marine mammal die-offs due to reduced prey
availability, fishery closures associated with harmful algal blooms, and declines in estuarine seagrass. The frequency and
intensity of marine heatwaves is increasing relative to historical baselines. They have occurred along all U.S. coasts, and
estuary temperature records show warm anomalies at the same time as offshore heatwaves. It is likely that already-seen
emergency responses such as changes to fishery season and catch limits, marketing of newly available or abundant
seafood species, or moving or harvesting aquaculture species before heat stress, will continue to be needed. Eventually
environmental management must shift from responding to events and adapt to new prevailing temperatures.

OPPORTUNITIES AND CHALLENGES

•	Warmer water or longer warm seasons may improve conditions for some species and boost some types of aquaculture.

•	Scientists are examining recruitment failures that are associated with above average temperature.

•	Heatwaves threaten the availability of culturally important foods, especially for indigenous populations.

•	Additional research is needed to understand how heat propagates from the sea and upstream in estuaries.

Assessment 1 3-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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POLICY CONTEXT AND QUESTIONS

Management must recognize that gradual water warming will be punctuated by heatwaves that can push systems past
thresholds. While short-duration events may function as sporadic shocks to coastal ecosystems from which recovery is
possible, longer lasting events will speed already-occurring ecosystem transitions. Coastal managers will need to evaluate
the cost-effectiveness and durability of temperature interventions such as habitat restoration and selective breeding and
cultivation of heat-resilient genotypes to resist ecological transitions.

Various regulatory and policy tools, such as threshold triggers or time/duration/frequency components in permits might help
meet water quality goals. Nevertheless, continued reductions to other stressors are needed to increase resiliency to extreme
oceanic events. Heatwaves and ocean warming may also change the ultimate attainability of water quality goals. This
scenario connects to sustainability goals for: zero hunger • decent work and economic growth • responsible consumption
and production • life below water.

SELECTED REFERENCES

Harvey, B. P., Marshall. K. E., Harley, C. D. G., & Russell, B. D. (2022). Predicting responses to marine heatwaves using
functional traits. Trends in ecology & evolution, 37(1), 20-29. https://doi.ora/10.1016/i.tree.2021.09.003

Smale, D.A., Wernberg, T., Oliver, E.C.J, et al. Marine heatwaves threaten global biodiversity and the provision of ecosystem
services. Nat. Clim. Chang. 9, 306-312 (2019). https://doi.ora/10.1038/s41558-019-0412-l

Pershing, A.J., K.E. Mills, A.M. Dayton, B.S. Franklin, and B.T. Kennedy. 2018. Evidence for adaptation from the 2016 marine
heatwave in the Northwest Atlantic Ocean. Oceanography 31 (21:152-161, https://doi.Org/l 0.5670/oceanoa.2018.213

Change in annual cumulative intensity of marine heatwaves in the U.S., 1982-2023 (https://www.epa.aov/climate-indicators/climate-
chanae-indicators-marine-heat-waves). Cumulative intensity is presented in degree days, which is equal to marine heatwave intensity
multiplied by duration. The red shaded areas experienced an increase in marine heatwave cumulative intensity, (Data Source: NOAA)


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Rising seas and floods threaten homes and businesses,
and consequently community viability. Adopting
floating building technologies would avoid damages
and enable continued investment in these places. They
can be an alternative to relocation and keep
neighborhoods intact.

TURNING TO FLOATING
BUILDINGS

COASTAL FUTURE

HOW DOES IT LOOK?

Increasing depths and frequency of
coastal flooding were making parts of
communities unviable. Repeatedly
attending to flood and storm
damages became unavoidable.

Many residents and businesses chose
to relocate; however, some saw
floating and amphibious structures as
a way to preserve their real estate
investments and remain in their
neighborhoods. Communities
embraced these buildings to sustain
flood-prone areas and establish new
developable spaces. Now, residential
and commercial uses are routinely
found in floating and amphibious
structures that safely rise above the
increasingly frequent coastal floods.

HOW DID IT HAPPEN?

Floating structures (located over
water) and amphibious structures (located on land) rely on a buoyant foundation and anchoring system. Enterprising
marinas began offering slips for floating structures, with the occupiable structure commonly built atop a barge or timber
foundation. Unlike houseboats, floating structures had no means of self-propulsion and are semi-permanently anchored.
Some floating and amphibious structures used hulls attached to stabilizing pylons that allow for vertical movement in-place.
Most were 1-3 stories, reflecting a delicate balance of buoyancy, stability, space layout, and even furniture placement.
Flexible, extra-long piping connected the structures to on-land utility networks by running below access piers. Wastewater
was typically stored in holding tanks and pumped from the structure to the on-land utility network.

HOW LIKELY iS IT?

While communities are very likely to explore adaptation options for flood-prone locations or seek to offset a lack of
developable land, floating and amphibious structures are unlikely to be widely adopted due to cost, complexity, and site
constraints. Floating and amphibious structures are typically located in areas with some protection from waves (e.g.,
sheltered marinas, rivers), limiting where they can be used. In areas where amphibious structures are suitable, home- and
businessowners are likely to be more comfortable with conventional fixed, elevated structures. In Europe, floating structures
have been developed as planned overwater neighborhoods to reduce project construction and maintenance costs,
whereas amphibious structures are less utilized. In the U.S., where existing floating structures are generally located in
marinas, it is unlikely that communities will expand into planned new neighborhoods. Floating casinos (so-called
"riverboats") are familiar in the U.S. There is currently a limited market for cruise ship apartments and floating and
amphibious homes and resorts which are oriented toward the luxury buyer, and it is unlikely that these setups will be
affordable options. This combination of cost and risk is thought to make it likely that individuals will opt for more
conventional, affordable options in established, safer areas. The strategy may have limited potential in single projects and
commercial uses.

Assessment 1 4-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	In communities with limited developable land, floating structures offer opportunities to accommodate sea level rise
within existing neighborhoods. Residents with strong community ties could remain although their home and
neighborhood would be radically reconfigured.

•	As with boats, floating structures will need regular hull maintenance. Similarly, indoor dampness, mold, and mildew will
need attention.

•	Structures may safely float but access in and out will be affected when roads and neighborhoods are flooded.

•	Floating and amphibious structures connect to on-land utility networks. Flood and storm damage (including on land)
may affect services, including the ability to pump wastewater. A strong concern is the accidental discharge of
untreated wastewater into waterways.

•	Buildings rise with floodwaters and rock with waves, so extreme storms, high winds, or large waves may lead to structural
and infrastructure damages or failure. Occupants who stay during storms may be at risk.

•	Owners could find that insurance is unavailable.

POLICY CONTEXT AND QUESTIONS

Land and water use conflicts involving recreation, public access, and scenic value interests are likely to stymie
development in high water use areas. Impacts to aquatic life must also be considered, particularly for floating structures
that affect light, wave energy, or bottom habitats.

As floating and amphibious
structures are necessarily within
floodplains or regulatory floodways,
their adoption requires a reimagining
of how communities conceive of
flood risk. Communities and states
may find that floating structures
stretch the limits of existing building
codes and land use regulations,
increasing the regulatory hurdles
and cost of construction. Further,
states and communities may find
that wastewater management and
the risk of accidental discharges are
counter to established water quality
and public health standards and
regulations. This scenario connects to
sustainability goals for: clean water
and sanitation • decent work and
economic growth • sustainable cities
and communities.

Floating homes in Amsterdam.

SELECTED REFERENCES

Penning-Rowseil, Edmund. Floating architecture in the landscape: climate change adaptation ideas, opportunities and
challenges. Landscape Research 45, no. 4 (2020): 395-411.

https://www.tandfonline.com/doi/full/10.1080/01426397.2Q19.1694881

Ontwikkelingscombinatie Waterbuurt West and Projectbureau IJburg of the Municipality of Amsterdam. Floating
Amsterdam: The development of IJbura's Waterbuurf. 2012.

Boiten raadgevende ingeniuers & Factor Architecten. Project review: Floating Homes 'De Gouden Kust,' Maasbommel, the
Netherlands, 1998-2005. 2011.


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Sea level rise with more frequent and severe storms are
leading to an increasingly loud call for coastal
engineering to prevent flooding and erosion. Accessing
and using beaches, piers, marinas, and ramps outside
of protective works can become difficult, and these
facilities will remain exposed to destructive storms.

LOSING WATERFRONT ACCESS

COASTAL FUTURE

HOW DOES IT LOOK?

Fishing, boating, sunbathing,
swimming, and other recreation
activities were an undeniable
draw to coastal places. As
threats from sea level rise and
worsening coastal storms
began accumulating, shoreline
communities turned more and
more to coastal engineering to
stay viable. Walls, levees, dikes,
and armoring were effective at
stopping flooding and erosion.
However, this security came at
the expense of the beaches,
swimming areas, piers, boat
ramps and marinas that were
left unprotected. They were out
of sight, difficult to access, and
eventually damaged or
squeezed out between water
side inundation and static land
side structures.

HOW DiD IT HAPPEN?

Coastal communities' main desires were to preserve homes and businesses and stabilize their shorelines. They protected
development on one side of an armored line. Sometimes strips of natural landscape (e.g., beach fills, living shorelines) were
employed as a buffer on the water side of the line. Without continual maintenance the artificial beaches and wetland
buffers were squeezed out against the walls and levees. Ocean beaches were more likely to be maintained in front of a
seawall than estuarine salt marsh in front of a floodwall because beaches were fundamental in the seaside communities. In
some cases, communities used networks of engineered structures, creating protective rings with combinations of levees,
floodwalls, seawalls, armored dunes, and sea gates. The structures had substantial height to protect from extreme storms.
These protective infrastructure rings became barriers to direct water access. Piers, boat ramps, and marinas were stranded
and forgotten outside of these rings. Some places had walkways atop levees and seawalls to preserve viewscapes,
otherwise the shoreline stayed out of sight. Plentiful access points were often provided for ocean beaches, but access to
the bayside shoreline was intermittent and direct access to the water may have been unavailable or required passing over
walls, down bulkheads, or across revetments.

HOW LIKELY IS IT?

Armoring has been a standard response to coastal hazards for centuries, in part because coastal roadways and other
coastal infrastructure were historically built without sea level rise in mind. Despite the high costs required for the installation
and maintenance of engineered structures, communities have continued to rely on armoring to protect existing
development. While there is some discourse about nature-based solutions, the evidence shows that shoreline communities
want (and are getting) levees, walls, tide gates, and so-called "dunes" that are vegetated sand veneers over steel or
concrete. In recent decades, some coastal states have begun to weigh the impacts of armoring against the potential loss

Assessment 1 5-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


-------
of public access to the shoreline. In part because of this concern, there has been pressure for sta tes to encourage
alternatives such as living shorelines, managed relocation, and retreat. However, because the threat of sea level rise to
public infrastructure and private property is intensifying, and so many concept plans for perimeter protection are on the
drawing boards, it is very likely that use of levees and walls will be widespread in densely populated areas, perhaps coupled
with some nature-based solutions. While many communities may attempt to preserve views with elevated boardwalks and
waterfront parks, it is very likely that easy public access to the water itself will be restricted, difficult or lost—especially on
highly developed estuarine shorelines.

OPPORTUNITIES AND CHALLENGES

•	Alternative adaptation measures, such as acquisition or rolling easements can protect public access to the shoreline.

•	Because armored shoreline structures may need to be rebuilt higher over time or may need to expand into adjacent
spaces, communities may come to regard public access as a transitory amenity.

•	Coastal communities may see decreased tourism if they are unable to maintain access ways to public recreation. For
communities that draw their identity from their proximity and access to coastal resources, this change will be profound.

•	Narrow "living shorelines" with no ability to migrate inland will have short lifespans unless regularly raised and renewed.
Breakwaters that are commonly co-installed with living shorelines will become submerged and can be a swimming or
boating hazard unless they are tended to as well.

POLICY CONTEXT AND QUESTIONS

As sea level rise and erosion continue on, more
communities may be drawn to invest in shoreline
engineering to protect existing development.
However, engineering solutions can negatively
impact public access. Stronger policies and
mechanisms may be needed, including strategies
like rolling easements. The loss of access to and use
of beaches, piers, and marinas, also raises concerns
that the populations which use these public resources
may not be the same segment of the public that
benefits from the protection of shoreline investments.

Maintaining recreation in and on the water is among
the reasons for the Clean Water Act, which states a
national goal that water quality will provide for those
activities. This scenario connects to sustainability
goals for: sustainable cities and communities.

SELECTED REFERENCES

Gittman, Rachel et al. (2015). Engineering away our
ngfurgl defenses: gn gnglvsis of shoreline hordening
in the US. Frontiers in Ecology and the Environment 13,
6 (2023): 301-307

Hgwgii Depgrtment of Lond grid Ngfurgl Resources.
Lorid Division. Howgii Coosfgl Lgnds Progrom. Hawaii
Coastal Erosion Management Plan. 2013.

US Army Corps of Engineers, Philodelphig District. New

Jersey Back Bays Coastal Storm Risk Management
Draft Integrated Feasibility Report and Tier I
Environmental Impact Statement. New Jersey Bgck
Bgys Study, 2021.

The U.S. Army Corps of Engineers' Philadelphia District constructs two new
sections of a seawall and rebuilds portions of the Atlantic City boardwalk
along the Absecon Inlet in New Jersey following coastal storm events. (Tim
Boyle, U.S. Army Corps of Engineers).


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

In much of the country warmer air and water
temperature are allowing boating to begin earlier in
the spring, and go longer into the fail. An extended
boating season will lead to greater environmental
impacts, and bring new ones as boats become a
presence in months when they had been absent.

EXTENDING THE BOATING

SEASON

COASTAL FUTURE

HOW DOES IT LOOK?
As global air and water
temperature kept warming,
the shoulder seasons for
boating kept extending.
Whereas in much of the
country Memorial Day and
Labor Day were previously
cultural markers opening and
closing the season, now
boating starts earlier and
ends later. This led to further
common boating impacts as
a result of more days on the
water. New ecological
problems also emerged as
boats became a presence in
what had been the off
season.

HOW DID IT HAPPEN?

Boaters continued to operate
earlier in the year as the

climate continued warming. Likewise, they stayed on the water later in the fall. The boating season grew significantly longer
than the three and a half months it had been from late May to early September.

Increasing the time that boaters and fishers, plus tour boats and seasonal ferries, were on the water simply added more
chances for routine impact from moorings, maintenance, trash and noise. Fuel spills, plus sewage and other discharges such
as graywater and bilgewater, increased proportionally. Shoreline erosion and anchoring impacts did too.

Management strategies for familiar impacts like seagrass damage, invasive species or interactions with marine mammals
needed more education and monitoring during longer seasons. New impacts also emerged from extended marina
operations. Fishing outside of traditional dates added pressures on species and carried the risk of exceeding annual fishery
allotments or activity in closed seasons. There was greater human presence during bird migration and breeding seasons
too.

HOW LIKELY IS IT?

In areas that have a traditional boating season of Memorial Day to Labor Day, a gradual extension of the boating season is
likely. Any extension to the boating season makes it likely that associated ecological impacts to habitat and water quality
and direct impacts to fish, migratory birds, and seagrass will be seen.

Other factors that may affect outcomes include whether more people will own boats if the season is longer.

Assessment 1 6-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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OPPORTUNITIES AND CHALLENGES

•	A longer season can place additional burdens on regulatory and safety agencies, and waterfront municipalities.

•	A longer season can bring positive effects for tourism and the marine trades.

•	Greater excise tax revenue may be available to fund conservation activities.

POLICY CONTEXT AND QUESTIONS

Fishery management may need to adjust quotas in recognition of longer seasons or for the temperature driven changes to
species presence. Further use of no-discharge zones which are designated areas where the discharge of both treated and
untreated sewage from vessels is prohibited can be one strategy when waters require additional protection. Having
pumpout stations where sewage holding tanks may be emptied is an accompanying technique. This scenario connects to
sustainability goals for: decent work and economic growth • life below water.

SELECTED REFERENCES

Carreno, A. & Lloret, J. (2021). Environmental Impacts of Increasing Leisure Boating Activity in Mediterranean Coastal
Waters. Ocean & Coastal Management, 209. https://doi.ora/] 0.1016/i.ocecoaman.2021.105693

About the Clean Boating Act (CBA) https://www.epa.aov/vessels-marinas-and-ports/about-clean-boatina-act-cba

A Recreational Boater's Guide to Vessel Sewage https://www.epa.aov/sites/default/files/2021-
06/documents/a recreational boaters guide to vessel sewaae.pdf


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Earth systems monitoring and future conditions
modeling yield a torrent of data about coastal
conditions. Alas it is beyond what humans can
comprehend and act on in real time. Artificial
intelligence systems are extending human capacity,
although turning to Al introduces technology risk.

TURNING TO ARTIFICIAL
INTELLIGENCE

COASTAL FUTURE
HOW DOES IT LOOK?

Environmental changes brought a myriad of challenges
to coastal management. Novel situations emerged and
long-standing problems were exacerbated. Stressors as
diverse as water temperature, precipitation and sea
level rise, increased the value of artificial intelligence
technology that integrated multiplying data streams,
helped with scenario analysis, predicted extreme
events, and analyzed monitoring results. Al became
more and more important for identifying risks and
implementing responses.

HOW DID IT HAPPEN?

Machine learning is a type of Al that recognizes patterns
in data, reduces time from data collection to forecasts,
can increase accuracy by using more data than models
(or humans) can, and synthesizes information to fill data
gaps. Generative Al uses neural networks to create text or image content. In the mid-2020s this technology became
mainstream through search and chat functions that fed it user prompts. Users became familiar with confabulations
(colloquially known as "hallucina tions") in which an Al synthesizes wholly fictional responses. Because Als were trained on
enormous datasets, they inherited the characteristics and biases of their input. For example, environmental models had
better representation of populated areas with rich data collection than other places.

As Al capability grew and managers became confident, processes were automated. Issuing weather outlooks and
warnings, rerouting shipping around marine mammals, anticipating and managing reservoir levels, opening and closing tide
gates, summoning law enforcement, controlling autonomous vehicles and ships, and numerous routine, mundane and
arcane tasks were taken over by Al and automation. Of course it was nearly impossible to understand how they worked.

HOW LIKELY IS II?

Al systems are already playing a role in science and
management. EPA scientists have been using
machine learning for quite some time and neural
networks are common in the sciences. U.S. Forest
Service used Al to help deploy firefighting resources.
The Department of Commerce's Artificial Intelligence
Al Use Case Inventory - 2022 (https://ai.aov/ai-use-
cases/), related examples of how NOAA used Al for:
analyzing acoustic data to detect whales and other
marine mammals, improving drought outlooks,
classifying land cover, preparing for coral bleaching,
identifying phytoplankton, detecting fog, forecasting
severe wind, hail and tornadoes, and making wave
observations, among other uses. It is very likely that Al
will have an even larger role in coastal management
as its capabilities increase and users gain
confidence.

NIST Al 600-1. Artificial Intelligence Risk Management Framework:
Generative Artificial Intelligence Profile

2.2. Confabulation

"Confabulation" refers to a phenomenon in which [Al] systems
generate and confidently present erroneous or false content in
response to prompts.... Confabulations are a natural result of the
way generative models are designed: they generate outputs
that approximate the statistical distribution of their training
data.... While such statistical prediction can produce factually
accurate and consistent outputs, it can also produce outputs
that are factually inaccurate or internally inconsistent. This
dynamic is particularly relevant when it comes to open-ended
prompts for long-form responses and in domains which require
highly contextual and/or domain expertise.... Risks from
confabulations may arise when users believe false content -
often due to the confident nature of the response - leading
users to act upon or promote the false information.

Assessment 1 7-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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It is very likely that Al systems will synthesize data streams and then implement procedures that have environmental
outcomes. While it is desirable to have humans in the loop, humans won't always have the ability to apprehend the data or
second guess an Al system, or will have lower skepticism about systems that have always performed well. Over time and
with wide use, errors and confabulations from Al are very likely. Risks will need to be continually monitored and mitigated.

OPPORTUNITIES AND CHALLENGES

•	Al can master the volume and types of data from satellites, instruments, drones and models that are too numerous for
humans to handle in real time.

•	Al is trained on pre-existing data, so results are most accurate when the current condition is representative of the data.

•	Using Al to supplement human skills and abilities can enlarge participation in the environmental workforce.

•	Al models are expensive to both develop and run, with high costs for research and training as well as high energy use.

POLICY CONTEXT AND
QUESTIONS

Risk management will be
essential and there is a high
need for systems around
the systems. Coastal
managers are going to
have to decide how much
autonomy for what types of
decisions they will grant to
Al and automation. There is
growing in terest in
regulations to govern Al
perils. This scenario
connects to sustainability
goals for: decent work and
economic growth •
industry, innovation, and
infrastructure • sustainable
cities and communities •
responsible consumption

and production life on	^ vas^	Qf platforms and data streams keep tabs on conditions and provides critical

iQr|d.	information. https://www.noaa.aov/exDlainers/monitorina-our-chanaina-world-from-land-sea-and-skv

SELECTED REFERENCES

U.S. Government Accountability Office (2023). Artificial Intelligence in Natural Hazard Modeling: Severe Storms, Hurricanes,
Floods, and Wildfires, https://www.aao.aov/products/aao-24-106213

The United Nations Educational, Scientific and Cultural Organization (2022). Fighting Climate Change with the Al for the
Planet Alliance, https://www.unesco.ora/en/articles/fiahtina-climate-chanae-ai-planet-alliance

National Institute of Standards and Technology (2024). Artificial Intelligence Risk Management Framework: Generative
Artificial Intelligence Profile. U.S. Department of Commerce, https://www.nist.aov/itl/ai-risk-manaaement-framework

OMB M24-10. Advancing Governance, Innovation, and Risk Management for Agency Use of Artificial Intelligence.

https://www.whitehouse.aov/omb/information-for-aaencies/memoranda/

air gap sensor

continuously operating
reference station

PORTS0
visibility
sensor

water level gauge

buoys:

ocean chemistry
wave sensors
water temperature gauge
meteorological sensors

monitoring

ATON mounted acoustic doppler current profiler

bottom mounted acoustic doppler current profiler

glider or autonomous
underwater vehicle


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CLIMATE READY

ESTUARIES

xvEPA

WHY THIS MATTERS

Storms and sea level rise combine to bring more
frequent costly events. As damages and repair bills
accumulate, eventually some will abandon their
houses. As they depart they will leave much behind—in
proven risky places. It will fall to local government to
clean up and restore these abandoned sites.

RESTORING ABANDONED SITES

COASTAL FUTURE

HOW DOES IT LOOK?

Sea level rise led to more frequent
high tide flooding and worsened the
impacts of coastal storms. The
endless cycle of floods, storms, and
repairs became financially and
emotionally burdensome for many
coastal residents. Eventually,
property owners began making ad
hoc decisions to relocate.
Abandoned property deteriorated
and led to adverse environmental
impacts.

HOW DiD IT HAPPEN?

Although residents of at-risk homes
hoped for protection, after damage
had already occurred many were
interested in buyouts. Yet it was
difficult to coordinate and operate
buyout programs even when
communities had funds available.

Without any assurance that their homes would be bought out and facing a long process regardless: unplanned retreat from
hazardous areas occurred whenever owners became unwilling or unable to bear the repeated repairs and accumulating
costs of recovering. Shouldering the cost became even more of a personal burden when private insurance companies
withdrew from the coastal market. Some states tried to fill the insurance gap, although policies were expensive due to small
risk pools and high-risk property.

Responsibility for cleanup and the cost of remediating public nuisance properties fell to health departments and
environmental agencies. Abandoned properties presented public health hazards due to septic systems, fuel tanks,
discarded pesticides, household chemicals, flood damaged vehicles, or asbestos building materials. Keeping building
debris from entering waterways posed further concerns. Attention to these matters was not a priority in lower-resourced
communities. The presence of vacant properties and derelict structures frequently had a negative effect on other residents'
desire to stay, perpetuating a cycle of abandonment.

When cleanups did occur, there was an opportunity for environmental restoration in lieu of reoccupation at these
demonstrated dangerous locations. However, land trusts and wildlife agencies had little interest in acquiring titles and
spending resources to restore habitat at small, random, dispersed sites.

HOW LIKELY IS IT?

It is very likely that coastal risks will increase in response to sea level rise and changes in extreme weather patterns. The U.S.
Congressional Budget Office estimates that homes outside of PEMA-designated Special Flood Hazard Areas will account for
approximately 40-50 percent of expected annual flood damage under a 2050 projection, making it likely that many
affected residents are unaware of flood risk, will not carry optional flood insurance, and will be less resilient to flood
damage. Additionally, insurance companies are withdrawing from increasingly hazardous coastal areas, leaving residents
to bear the full risk of storms.

Assessment 1 8-2025
Foreseeing Coastal Change To Strategically Guide Adaptation, EPA 840R25001


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Some federal agencies offer property buyout programs, although historically projects have typically been small, targeting
only a few individual properties. It is very unlikely that everyone who becomes interested in a buyout will be
accommodated. Jurisdictions in higher-income and denser counties are more likely to conduct buyouts. It is about an even
chance that rural coastal areas will see some abandonment. Abandonment is not a novel reaction: abandoned buildings
are easily found in the U.S., and this country has a notable number of ghost towns.

Since property in good condition is very unlikely to be abandoned, where there are abandoned sites they are very likely to
pose environmental problems, become nuisances, and need cleanup and demolition. Without a process to structure an
ownership transfer, abandoned property is very likely to remain neglected. Even if a buyout acquisition is completed, land-
use analysis of past FEMA-funded buyout sites suggests that ecological restoration occurs infrequently.

OPPORTUNITIES AND CHALLENGES

•	Federal programs for buyouts typically require the permanent conversion of buyout sites to open space or other
floodplain compatible uses.

•	Restoration of small, dispersed sites can still produce meaningful ecological benefits (i.e., wildlife habitat, wildlife
corridors and linkages, flood storage). Future buyouts in the same area offer the potential to restore larger tracts.

POLICY CONTEXT AND QUESTIONS

Relocation from coastal hazards in the U.S. is primarily facilitated
by post-disaster federal- and state-funded buyout programs,
sometimes with local match, which results in an ad hoc approach
that is difficult to predict. Restoration and reuse of buyout sites
may challenge less affluent communities, where acquiring,
restoring and maintaining land may be perceived as a burden.

Disaster victims will not be alone in making decisions to withdraw
from coastal risk. Local governments will assess their legal
obligation to maintain, repair, and upgrade vulnerable roads and
infrastructure. This could be another push factor. Pre-disaster
planning, which could include targeted or wholesale relocation,
can help create a transparent dialogue between local
governments and residents to ultimately limit outmigration,
encourage local resettlement where appropriate, and maintain a
sense of community.

This scenario connects to sustainability goals for: no poverty • good health and well-being • reduced inequalities •
sustainable cities and communities • life below water • life on land.

SELECTED REFERENCES

EPA Toolkit about Abandoned Mobile Homes, https://www.epa.aov/smm/toolkit-about-abandoned-mobile-homes

Congressional Research Service. 2024. Floodplain Buyouts: Federal Funding for Property Acquisition.

https://crsreports.conaress.aov/product/pdf/IN/INl 1911

Mach, K. J., Kraan, C. M., Hino, M., Siders, A. R., Johnston, E. M., & Field, C. B. (2019). Managed retreat through voluntary
buyouts of flood-prone properties. Science Advances, 5(10).

Anurodhg Mukherji, Ke'Ziygh Willigmson, Koyode Nelson Adeniji, Milleo Meghgn, Scott Curtis, Bello Sgrding, 2024. Buyouts in
the Corolinos: Pre & Post buyout perspectives of public officiols gnd community leoders. International Journal of Disaster Risk
Reduction, Volume 113. https://doi.ora/10.1016/i.iidrr.2024.104906.

Volunteers help after a hurricane. FEMA/Marvin Nauman


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