Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United States

Abstract Coastal wetlands have two dimensions of vulnerability to sea‐level rise (SLR), a vertical one, in cases where SLR outpaces their capacity to vertically accrete, and a lateral one, in cases where they are restricted from migrating inland by topography and land use. We conducted a meta‐analys...

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Main Authors: James R. Holmquist, Lauren N. Brown, Glen M. MacDonald
Format: Article
Language:English
Published: Wiley 2021-06-01
Series:Earth's Future
Subjects:
Online Access:https://doi.org/10.1029/2020EF001804
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author James R. Holmquist
Lauren N. Brown
Glen M. MacDonald
author_facet James R. Holmquist
Lauren N. Brown
Glen M. MacDonald
author_sort James R. Holmquist
collection DOAJ
description Abstract Coastal wetlands have two dimensions of vulnerability to sea‐level rise (SLR), a vertical one, in cases where SLR outpaces their capacity to vertically accrete, and a lateral one, in cases where they are restricted from migrating inland by topography and land use. We conducted a meta‐analysis of accretion rates, standardized our analysis by using only 137Cs based estimates, and used model intercomparison to generate a vertical resilience index, a function of local SLR, tidal range, and tidal elevation category for the tidal wetlands of the contiguous US. We paired the vertical resilience index with a lateral resilience index made up of elevation, water level, and land cover maps, then projected them both into the future using localized SLR scenarios. At the regional scale, the vertical resilience index predicts changes from marsh aggradation to submergence for the coastal US Mid‐Atlantic, Southeast, and portions of the Northeast by 2100. At the sub‐regional scale, there is a geographic tradeoff between vertical and lateral resilience with more northerly wetlands vulnerable to the lack of suitable proportional area to migrate into, and more southerly wetlands vulnerable to accretion deficit. We estimate between 43% and 48% of the existing contiguous US wetland area, almost entirely located in watersheds along the Gulf of Mexico and Mid‐Atlantic coasts, is subject to both vertical and lateral limitations. These vertical and lateral resilience indices could help direct future research, planning, and mitigation efforts at a national scale, as well as supplement more processed informed approaches by local planners and practitioners.
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spelling doaj.art-c2523513038a40379e454edb90cce8ea2022-12-22T03:41:39ZengWileyEarth's Future2328-42772021-06-0196n/an/a10.1029/2020EF001804Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United StatesJames R. Holmquist0Lauren N. Brown1Glen M. MacDonald2Smithsonian Environmental Research Center Edgewater MD USADepartment of Geography University of California, Los Angeles Los Angeles CA USADepartment of Geography University of California, Los Angeles Los Angeles CA USAAbstract Coastal wetlands have two dimensions of vulnerability to sea‐level rise (SLR), a vertical one, in cases where SLR outpaces their capacity to vertically accrete, and a lateral one, in cases where they are restricted from migrating inland by topography and land use. We conducted a meta‐analysis of accretion rates, standardized our analysis by using only 137Cs based estimates, and used model intercomparison to generate a vertical resilience index, a function of local SLR, tidal range, and tidal elevation category for the tidal wetlands of the contiguous US. We paired the vertical resilience index with a lateral resilience index made up of elevation, water level, and land cover maps, then projected them both into the future using localized SLR scenarios. At the regional scale, the vertical resilience index predicts changes from marsh aggradation to submergence for the coastal US Mid‐Atlantic, Southeast, and portions of the Northeast by 2100. At the sub‐regional scale, there is a geographic tradeoff between vertical and lateral resilience with more northerly wetlands vulnerable to the lack of suitable proportional area to migrate into, and more southerly wetlands vulnerable to accretion deficit. We estimate between 43% and 48% of the existing contiguous US wetland area, almost entirely located in watersheds along the Gulf of Mexico and Mid‐Atlantic coasts, is subject to both vertical and lateral limitations. These vertical and lateral resilience indices could help direct future research, planning, and mitigation efforts at a national scale, as well as supplement more processed informed approaches by local planners and practitioners.https://doi.org/10.1029/2020EF001804coastal wetlandaccretionrelative sea‐level riselateral migration
spellingShingle James R. Holmquist
Lauren N. Brown
Glen M. MacDonald
Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United States
Earth's Future
coastal wetland
accretion
relative sea‐level rise
lateral migration
title Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United States
title_full Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United States
title_fullStr Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United States
title_full_unstemmed Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United States
title_short Localized Scenarios and Latitudinal Patterns of Vertical and Lateral Resilience of Tidal Marshes to Sea‐Level Rise in the Contiguous United States
title_sort localized scenarios and latitudinal patterns of vertical and lateral resilience of tidal marshes to sea level rise in the contiguous united states
topic coastal wetland
accretion
relative sea‐level rise
lateral migration
url https://doi.org/10.1029/2020EF001804
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