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Predicted Sea‐Level Rise‐Driven Biogeomorphological Changes on Fire Island, New York: Implications for People and Plovers
Forecasting biogeomorphological conditions for barrier islands is critical for informing sea‐level rise (SLR) planning, including management of coastal development and ecosystems. We combined five probabilistic models to predict SLR‐driven changes and their implications on Fire Island, New York, by...
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Published in: | Earth's future 2022-04, Vol.10 (4), p.n/a |
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description | Forecasting biogeomorphological conditions for barrier islands is critical for informing sea‐level rise (SLR) planning, including management of coastal development and ecosystems. We combined five probabilistic models to predict SLR‐driven changes and their implications on Fire Island, New York, by 2050. We predicted barrier island biogeomorphological conditions, dynamic landcover response, piping plover (Charadrius melodus) habitat availability, and probability of storm overwash under three scenarios of shoreline change (SLC) and compared results to observed 2014/2015 conditions. Scenarios assumed increasing rates of mean SLC from 0 to 4.71 m erosion per year. We observed uncertainty in several morphological predictions (e.g., beach width, dune height), suggesting decreasing confidence that Fire Island will evolve in response to SLR as it has in the past. Where most likely conditions could be determined, models predicted that Fire Island would become flatter, narrower, and more overwash‐prone with increasing rates of SLC. Beach ecosystems were predicted to respond dynamically to SLR and migrate with the shoreline, while marshes lost the most area of any landcover type compared to 2014/2015 conditions. Such morphological changes may lead to increased flooding or breaching with coastal storms. However—although modest declines in piping plover habitat were observed with SLC—the dynamic response of beaches, flatter topography, and increased likelihood of overwash suggest storms could promote suitable conditions for nesting piping plovers above what our geomorphology models predict. Therefore, Fire Island may offer a conservation opportunity for coastal species that rely on early successional beach environments if natural overwash processes are encouraged.
Plain Language Summary
Predicting a barrier island's future characteristics is important for planning, particularly given that these areas contain habitats used by threatened and endangered species and are popular sites for housing and recreation. In this study, we combined five models to predict barrier island characteristics like elevation, beach width, and dune height under three rates of shoreline erosion at Fire Island, New York. Models were also used to predict how likely parts of the island were to be permanently flooded by sea‐level rise or to experience overwash with storms, where waves move sand deeper into the island. We found that Fire Island would likely become narrower and flatter while experie |
doi_str_mv | 10.1029/2021EF002436 |
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Plain Language Summary
Predicting a barrier island's future characteristics is important for planning, particularly given that these areas contain habitats used by threatened and endangered species and are popular sites for housing and recreation. In this study, we combined five models to predict barrier island characteristics like elevation, beach width, and dune height under three rates of shoreline erosion at Fire Island, New York. Models were also used to predict how likely parts of the island were to be permanently flooded by sea‐level rise or to experience overwash with storms, where waves move sand deeper into the island. We found that Fire Island would likely become narrower and flatter while experiencing more overwash with storms as rates of shoreline erosion increase. These changes may lead to more flooding in housing communities and businesses on the island. However, models also predicted that beach habitats used by shorebirds like the piping plover would not flood permanently. Instead, they would move as the shoreline changes position as long as human structures like buildings or seawalls do not block sand movement. This migration of beaches and sand is important, as it also allows a barrier island to evolve and survive with rising sea levels.
Key Points
With increasing shoreline erosion and landward retreat, Fire Island was predicted to become flatter, narrower, and more overwash‐prone
Beaches are expected to be least impacted and to replace other landcover types as they migrate with the shoreline
Habitats used by piping plovers are expected to persist as long as development and stabilization structures do not limit beach migration</description><identifier>ISSN: 2328-4277</identifier><identifier>EISSN: 2328-4277</identifier><identifier>DOI: 10.1029/2021EF002436</identifier><language>eng</language><publisher>Bognor Regis: John Wiley & Sons, Inc</publisher><subject>barrier island ; Barrier islands ; Beaches ; Biological effects ; Birds ; Coastal development ; Coastal flooding ; coastal habitats ; Coastal management ; Coastal morphology ; Coastal storms ; Coasts ; Conservation ; Dynamic response ; Ecosystems ; Environment models ; erosion ; Flooding ; Floods ; Geomorphology ; Habitat availability ; Marshes ; Mathematical models ; Nesting ; Piping ; Probabilistic models ; sea level rise ; Sediments ; shorebirds ; Shoreline protection ; Shorelines ; Soil erosion ; Statistical analysis ; Storms ; Strategic management</subject><ispartof>Earth's future, 2022-04, Vol.10 (4), p.n/a</ispartof><rights>Published 2022. This article is a U.S. Government work and is in the public domain in the USA.</rights><rights>2022. This work is published under http://creativecommons.org/licenses/by-nc/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3941-8383872e0c29ce0b1c4720dc054f8c7ffb2d5b804308b1cfc1558b69a66e325d3</citedby><cites>FETCH-LOGICAL-a3941-8383872e0c29ce0b1c4720dc054f8c7ffb2d5b804308b1cfc1558b69a66e325d3</cites><orcidid>0000-0001-8050-5727 ; 0000-0002-1879-7893 ; 0000-0002-0621-8954 ; 0000-0002-2420-3115 ; 0000-0002-5703-5672 ; 0000-0002-5472-769X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2655589576/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2655589576?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,11562,25753,27924,27925,37012,44590,46052,46476,75126</link.rule.ids></links><search><creatorcontrib>Zeigler, S. L.</creatorcontrib><creatorcontrib>Gutierrez, B. T.</creatorcontrib><creatorcontrib>Lentz, E. E.</creatorcontrib><creatorcontrib>Plant, N. G.</creatorcontrib><creatorcontrib>Sturdivant, E. J.</creatorcontrib><creatorcontrib>Doran, K. S.</creatorcontrib><title>Predicted Sea‐Level Rise‐Driven Biogeomorphological Changes on Fire Island, New York: Implications for People and Plovers</title><title>Earth's future</title><description>Forecasting biogeomorphological conditions for barrier islands is critical for informing sea‐level rise (SLR) planning, including management of coastal development and ecosystems. We combined five probabilistic models to predict SLR‐driven changes and their implications on Fire Island, New York, by 2050. We predicted barrier island biogeomorphological conditions, dynamic landcover response, piping plover (Charadrius melodus) habitat availability, and probability of storm overwash under three scenarios of shoreline change (SLC) and compared results to observed 2014/2015 conditions. Scenarios assumed increasing rates of mean SLC from 0 to 4.71 m erosion per year. We observed uncertainty in several morphological predictions (e.g., beach width, dune height), suggesting decreasing confidence that Fire Island will evolve in response to SLR as it has in the past. Where most likely conditions could be determined, models predicted that Fire Island would become flatter, narrower, and more overwash‐prone with increasing rates of SLC. Beach ecosystems were predicted to respond dynamically to SLR and migrate with the shoreline, while marshes lost the most area of any landcover type compared to 2014/2015 conditions. Such morphological changes may lead to increased flooding or breaching with coastal storms. However—although modest declines in piping plover habitat were observed with SLC—the dynamic response of beaches, flatter topography, and increased likelihood of overwash suggest storms could promote suitable conditions for nesting piping plovers above what our geomorphology models predict. Therefore, Fire Island may offer a conservation opportunity for coastal species that rely on early successional beach environments if natural overwash processes are encouraged.
Plain Language Summary
Predicting a barrier island's future characteristics is important for planning, particularly given that these areas contain habitats used by threatened and endangered species and are popular sites for housing and recreation. In this study, we combined five models to predict barrier island characteristics like elevation, beach width, and dune height under three rates of shoreline erosion at Fire Island, New York. Models were also used to predict how likely parts of the island were to be permanently flooded by sea‐level rise or to experience overwash with storms, where waves move sand deeper into the island. We found that Fire Island would likely become narrower and flatter while experiencing more overwash with storms as rates of shoreline erosion increase. These changes may lead to more flooding in housing communities and businesses on the island. However, models also predicted that beach habitats used by shorebirds like the piping plover would not flood permanently. Instead, they would move as the shoreline changes position as long as human structures like buildings or seawalls do not block sand movement. This migration of beaches and sand is important, as it also allows a barrier island to evolve and survive with rising sea levels.
Key Points
With increasing shoreline erosion and landward retreat, Fire Island was predicted to become flatter, narrower, and more overwash‐prone
Beaches are expected to be least impacted and to replace other landcover types as they migrate with the shoreline
Habitats used by piping plovers are expected to persist as long as development and stabilization structures do not limit beach migration</description><subject>barrier island</subject><subject>Barrier islands</subject><subject>Beaches</subject><subject>Biological effects</subject><subject>Birds</subject><subject>Coastal development</subject><subject>Coastal flooding</subject><subject>coastal habitats</subject><subject>Coastal management</subject><subject>Coastal morphology</subject><subject>Coastal storms</subject><subject>Coasts</subject><subject>Conservation</subject><subject>Dynamic response</subject><subject>Ecosystems</subject><subject>Environment models</subject><subject>erosion</subject><subject>Flooding</subject><subject>Floods</subject><subject>Geomorphology</subject><subject>Habitat availability</subject><subject>Marshes</subject><subject>Mathematical models</subject><subject>Nesting</subject><subject>Piping</subject><subject>Probabilistic models</subject><subject>sea level rise</subject><subject>Sediments</subject><subject>shorebirds</subject><subject>Shoreline protection</subject><subject>Shorelines</subject><subject>Soil erosion</subject><subject>Statistical analysis</subject><subject>Storms</subject><subject>Strategic management</subject><issn>2328-4277</issn><issn>2328-4277</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNp9kc9OGzEQxldVkYootz6AJa6k-M-uveYGaUIjRRABPfRkeb2zwamzs7VDEAekPkKfkSfBJVXFqfbB45mfvm80UxSfGP3MKNcnnHI2mVLKSyHfFftc8HpUcqXev4k_FIcprWg-WlFRqf3iaRGh9W4DLbkB-_zr9xy2EMi1T5A_X6LfQk_OPS4B1xiHOwy49M4GMr6z_RISwZ5MfQQyS8H27TG5hAfyHeOPUzJbDyGjG499Ih1GsgAcApCMkUXALcT0sdjrbEhw-Pc9KL5NJ7fjr6P51cVsfDYfWaFLNqpFvooDdVw7oA1zpeK0dbQqu9qprmt4WzU1LQWtc7FzrKrqRmorJQheteKgmO10W7QrM0S_tvHRoPXmNYFxaWzceBfASMt1o9qGOlWWDEQN0AjJZB6vtsrWWetopzVE_HkPaWNWeB_73L7hssrGulIyU8c7ykVMKUL3z5VR82df5u2-Ms52-IMP8Phf1kymt1xrJl4Aud2Wtg</recordid><startdate>202204</startdate><enddate>202204</enddate><creator>Zeigler, S. 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L. ; Gutierrez, B. T. ; Lentz, E. E. ; Plant, N. G. ; Sturdivant, E. J. ; Doran, K. 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S.</creatorcontrib><collection>Wiley Online Library Open Access</collection><collection>Wiley Journals</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Publicly Available Content (ProQuest)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><collection>Environment Abstracts</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Earth's future</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zeigler, S. L.</au><au>Gutierrez, B. T.</au><au>Lentz, E. E.</au><au>Plant, N. G.</au><au>Sturdivant, E. J.</au><au>Doran, K. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Predicted Sea‐Level Rise‐Driven Biogeomorphological Changes on Fire Island, New York: Implications for People and Plovers</atitle><jtitle>Earth's future</jtitle><date>2022-04</date><risdate>2022</risdate><volume>10</volume><issue>4</issue><epage>n/a</epage><issn>2328-4277</issn><eissn>2328-4277</eissn><abstract>Forecasting biogeomorphological conditions for barrier islands is critical for informing sea‐level rise (SLR) planning, including management of coastal development and ecosystems. We combined five probabilistic models to predict SLR‐driven changes and their implications on Fire Island, New York, by 2050. We predicted barrier island biogeomorphological conditions, dynamic landcover response, piping plover (Charadrius melodus) habitat availability, and probability of storm overwash under three scenarios of shoreline change (SLC) and compared results to observed 2014/2015 conditions. Scenarios assumed increasing rates of mean SLC from 0 to 4.71 m erosion per year. We observed uncertainty in several morphological predictions (e.g., beach width, dune height), suggesting decreasing confidence that Fire Island will evolve in response to SLR as it has in the past. Where most likely conditions could be determined, models predicted that Fire Island would become flatter, narrower, and more overwash‐prone with increasing rates of SLC. Beach ecosystems were predicted to respond dynamically to SLR and migrate with the shoreline, while marshes lost the most area of any landcover type compared to 2014/2015 conditions. Such morphological changes may lead to increased flooding or breaching with coastal storms. However—although modest declines in piping plover habitat were observed with SLC—the dynamic response of beaches, flatter topography, and increased likelihood of overwash suggest storms could promote suitable conditions for nesting piping plovers above what our geomorphology models predict. Therefore, Fire Island may offer a conservation opportunity for coastal species that rely on early successional beach environments if natural overwash processes are encouraged.
Plain Language Summary
Predicting a barrier island's future characteristics is important for planning, particularly given that these areas contain habitats used by threatened and endangered species and are popular sites for housing and recreation. In this study, we combined five models to predict barrier island characteristics like elevation, beach width, and dune height under three rates of shoreline erosion at Fire Island, New York. Models were also used to predict how likely parts of the island were to be permanently flooded by sea‐level rise or to experience overwash with storms, where waves move sand deeper into the island. We found that Fire Island would likely become narrower and flatter while experiencing more overwash with storms as rates of shoreline erosion increase. These changes may lead to more flooding in housing communities and businesses on the island. However, models also predicted that beach habitats used by shorebirds like the piping plover would not flood permanently. Instead, they would move as the shoreline changes position as long as human structures like buildings or seawalls do not block sand movement. This migration of beaches and sand is important, as it also allows a barrier island to evolve and survive with rising sea levels.
Key Points
With increasing shoreline erosion and landward retreat, Fire Island was predicted to become flatter, narrower, and more overwash‐prone
Beaches are expected to be least impacted and to replace other landcover types as they migrate with the shoreline
Habitats used by piping plovers are expected to persist as long as development and stabilization structures do not limit beach migration</abstract><cop>Bognor Regis</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1029/2021EF002436</doi><tpages>25</tpages><orcidid>https://orcid.org/0000-0001-8050-5727</orcidid><orcidid>https://orcid.org/0000-0002-1879-7893</orcidid><orcidid>https://orcid.org/0000-0002-0621-8954</orcidid><orcidid>https://orcid.org/0000-0002-2420-3115</orcidid><orcidid>https://orcid.org/0000-0002-5703-5672</orcidid><orcidid>https://orcid.org/0000-0002-5472-769X</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | barrier island Barrier islands Beaches Biological effects Birds Coastal development Coastal flooding coastal habitats Coastal management Coastal morphology Coastal storms Coasts Conservation Dynamic response Ecosystems Environment models erosion Flooding Floods Geomorphology Habitat availability Marshes Mathematical models Nesting Piping Probabilistic models sea level rise Sediments shorebirds Shoreline protection Shorelines Soil erosion Statistical analysis Storms Strategic management |
title | Predicted Sea‐Level Rise‐Driven Biogeomorphological Changes on Fire Island, New York: Implications for People and Plovers |
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