Hurricane Sandy’s flood frequency increasing from year 1800 to 2100
Coastal flood hazard varies in response to changes in storm surge climatology and the sea level. Here we combine probabilistic projections of the sea level and storm surge climatology to estimate the temporal evolution of flood hazard. We find that New York City’s flood hazard has increased signific...
Gespeichert in:
Veröffentlicht in: | Proceedings of the National Academy of Sciences - PNAS 2016-10, Vol.113 (43), p.12071-12075 |
---|---|
Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 12075 |
---|---|
container_issue | 43 |
container_start_page | 12071 |
container_title | Proceedings of the National Academy of Sciences - PNAS |
container_volume | 113 |
creator | Lin, Ning Kopp, Robert E. Horton, Benjamin P. Donnelly, Jeffrey P. |
description | Coastal flood hazard varies in response to changes in storm surge climatology and the sea level. Here we combine probabilistic projections of the sea level and storm surge climatology to estimate the temporal evolution of flood hazard. We find that New York City’s flood hazard has increased significantly over the past two centuries and is very likely to increase more sharply over the 21st century. Due to the effect of sea level rise, the return period of Hurricane Sandy’s flood height decreased by a factor of ∼3× from year 1800 to 2000 and is estimated to decrease by a further ∼4.4× from 2000 to 2100 under a moderate-emissions pathway. When potential storm climatology change over the 21st century is also accounted for, Sandy’s return period is estimated to decrease by ∼3× to 17× from 2000 to 2100. |
doi_str_mv | 10.1073/pnas.1604386113 |
format | Article |
fullrecord | <record><control><sourceid>jstor_pubme</sourceid><recordid>TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5087008</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>26472203</jstor_id><sourcerecordid>26472203</sourcerecordid><originalsourceid>FETCH-LOGICAL-a532t-c4e2dcab8df40b1ad1b62dcb7a3fe0e77b04b90754a80a64349a7f06e0dbabc3</originalsourceid><addsrcrecordid>eNpdkctuFDEQRS1ERIbAmhWoJTZsOik_2o8NEooCiRSJBdlbZbc79KjHHuzuSLPjN_g9vgSHCXmwKunWqau6uoS8oXBMQfGTbcRyTCUIriWl_BlZUTC0lcLAc7ICYKrVgolD8rKUNQCYTsMLcsiUMmAMW5Gz8yXn0WMMzTeM_e73z1-lGaaU-mbI4ccSot81Y_Q5YBnjdRXTptkFzA3VAM2cGkYBXpGDAacSXt_NI3L1-ezq9Ly9_Prl4vTTZYsdZ3PrRWC9R6f7QYCj2FMnq-AU8iFAUMqBcAZUJ1ADSsGFQTWADNA7dJ4fkY972-3iNqH3Ic4ZJ7vN4wbzziYc7dNNHL_b63RjO9AKQFeDD3cGOdVsZbabsfgwTTV_WoqlmndSc-igou__Q9dpybGm-0sZJikTlTrZUz6nUnIY7p-hYG8bsrcN2YeG6sW7xxnu-X-VVODtHliXOeWHvRSKMeD8D1hvlus</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1835926124</pqid></control><display><type>article</type><title>Hurricane Sandy’s flood frequency increasing from year 1800 to 2100</title><source>JSTOR Archive Collection A-Z Listing</source><source>PubMed Central</source><source>Alma/SFX Local Collection</source><source>Free Full-Text Journals in Chemistry</source><creator>Lin, Ning ; Kopp, Robert E. ; Horton, Benjamin P. ; Donnelly, Jeffrey P.</creator><creatorcontrib>Lin, Ning ; Kopp, Robert E. ; Horton, Benjamin P. ; Donnelly, Jeffrey P.</creatorcontrib><description>Coastal flood hazard varies in response to changes in storm surge climatology and the sea level. Here we combine probabilistic projections of the sea level and storm surge climatology to estimate the temporal evolution of flood hazard. We find that New York City’s flood hazard has increased significantly over the past two centuries and is very likely to increase more sharply over the 21st century. Due to the effect of sea level rise, the return period of Hurricane Sandy’s flood height decreased by a factor of ∼3× from year 1800 to 2000 and is estimated to decrease by a further ∼4.4× from 2000 to 2100 under a moderate-emissions pathway. When potential storm climatology change over the 21st century is also accounted for, Sandy’s return period is estimated to decrease by ∼3× to 17× from 2000 to 2100.</description><identifier>ISSN: 0027-8424</identifier><identifier>EISSN: 1091-6490</identifier><identifier>DOI: 10.1073/pnas.1604386113</identifier><identifier>PMID: 27790992</identifier><language>eng</language><publisher>United States: National Academy of Sciences</publisher><subject>Climate ; Floods ; Hazards ; Hurricanes ; Physical Sciences ; Sea level ; Tidal waves</subject><ispartof>Proceedings of the National Academy of Sciences - PNAS, 2016-10, Vol.113 (43), p.12071-12075</ispartof><rights>Volumes 1–89 and 106–113, copyright as a collective work only; author(s) retains copyright to individual articles</rights><rights>Copyright National Academy of Sciences Oct 25, 2016</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a532t-c4e2dcab8df40b1ad1b62dcb7a3fe0e77b04b90754a80a64349a7f06e0dbabc3</citedby><cites>FETCH-LOGICAL-a532t-c4e2dcab8df40b1ad1b62dcb7a3fe0e77b04b90754a80a64349a7f06e0dbabc3</cites><orcidid>0000-0002-5571-1606 ; 0000-0003-4016-9428</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26472203$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26472203$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,727,780,784,803,885,27924,27925,53791,53793,58017,58250</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/27790992$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Lin, Ning</creatorcontrib><creatorcontrib>Kopp, Robert E.</creatorcontrib><creatorcontrib>Horton, Benjamin P.</creatorcontrib><creatorcontrib>Donnelly, Jeffrey P.</creatorcontrib><title>Hurricane Sandy’s flood frequency increasing from year 1800 to 2100</title><title>Proceedings of the National Academy of Sciences - PNAS</title><addtitle>Proc Natl Acad Sci U S A</addtitle><description>Coastal flood hazard varies in response to changes in storm surge climatology and the sea level. Here we combine probabilistic projections of the sea level and storm surge climatology to estimate the temporal evolution of flood hazard. We find that New York City’s flood hazard has increased significantly over the past two centuries and is very likely to increase more sharply over the 21st century. Due to the effect of sea level rise, the return period of Hurricane Sandy’s flood height decreased by a factor of ∼3× from year 1800 to 2000 and is estimated to decrease by a further ∼4.4× from 2000 to 2100 under a moderate-emissions pathway. When potential storm climatology change over the 21st century is also accounted for, Sandy’s return period is estimated to decrease by ∼3× to 17× from 2000 to 2100.</description><subject>Climate</subject><subject>Floods</subject><subject>Hazards</subject><subject>Hurricanes</subject><subject>Physical Sciences</subject><subject>Sea level</subject><subject>Tidal waves</subject><issn>0027-8424</issn><issn>1091-6490</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNpdkctuFDEQRS1ERIbAmhWoJTZsOik_2o8NEooCiRSJBdlbZbc79KjHHuzuSLPjN_g9vgSHCXmwKunWqau6uoS8oXBMQfGTbcRyTCUIriWl_BlZUTC0lcLAc7ICYKrVgolD8rKUNQCYTsMLcsiUMmAMW5Gz8yXn0WMMzTeM_e73z1-lGaaU-mbI4ccSot81Y_Q5YBnjdRXTptkFzA3VAM2cGkYBXpGDAacSXt_NI3L1-ezq9Ly9_Prl4vTTZYsdZ3PrRWC9R6f7QYCj2FMnq-AU8iFAUMqBcAZUJ1ADSsGFQTWADNA7dJ4fkY972-3iNqH3Ic4ZJ7vN4wbzziYc7dNNHL_b63RjO9AKQFeDD3cGOdVsZbabsfgwTTV_WoqlmndSc-igou__Q9dpybGm-0sZJikTlTrZUz6nUnIY7p-hYG8bsrcN2YeG6sW7xxnu-X-VVODtHliXOeWHvRSKMeD8D1hvlus</recordid><startdate>20161025</startdate><enddate>20161025</enddate><creator>Lin, Ning</creator><creator>Kopp, Robert E.</creator><creator>Horton, Benjamin P.</creator><creator>Donnelly, Jeffrey P.</creator><general>National Academy of Sciences</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QG</scope><scope>7QL</scope><scope>7QP</scope><scope>7QR</scope><scope>7SN</scope><scope>7SS</scope><scope>7T5</scope><scope>7TK</scope><scope>7TM</scope><scope>7TO</scope><scope>7U9</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>H94</scope><scope>M7N</scope><scope>P64</scope><scope>RC3</scope><scope>7X8</scope><scope>5PM</scope><orcidid>https://orcid.org/0000-0002-5571-1606</orcidid><orcidid>https://orcid.org/0000-0003-4016-9428</orcidid></search><sort><creationdate>20161025</creationdate><title>Hurricane Sandy’s flood frequency increasing from year 1800 to 2100</title><author>Lin, Ning ; Kopp, Robert E. ; Horton, Benjamin P. ; Donnelly, Jeffrey P.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a532t-c4e2dcab8df40b1ad1b62dcb7a3fe0e77b04b90754a80a64349a7f06e0dbabc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Climate</topic><topic>Floods</topic><topic>Hazards</topic><topic>Hurricanes</topic><topic>Physical Sciences</topic><topic>Sea level</topic><topic>Tidal waves</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lin, Ning</creatorcontrib><creatorcontrib>Kopp, Robert E.</creatorcontrib><creatorcontrib>Horton, Benjamin P.</creatorcontrib><creatorcontrib>Donnelly, Jeffrey P.</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>Animal Behavior Abstracts</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Calcium & Calcified Tissue Abstracts</collection><collection>Chemoreception Abstracts</collection><collection>Ecology Abstracts</collection><collection>Entomology Abstracts (Full archive)</collection><collection>Immunology Abstracts</collection><collection>Neurosciences Abstracts</collection><collection>Nucleic Acids Abstracts</collection><collection>Oncogenes and Growth Factors Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Genetics Abstracts</collection><collection>MEDLINE - Academic</collection><collection>PubMed Central (Full Participant titles)</collection><jtitle>Proceedings of the National Academy of Sciences - PNAS</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lin, Ning</au><au>Kopp, Robert E.</au><au>Horton, Benjamin P.</au><au>Donnelly, Jeffrey P.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hurricane Sandy’s flood frequency increasing from year 1800 to 2100</atitle><jtitle>Proceedings of the National Academy of Sciences - PNAS</jtitle><addtitle>Proc Natl Acad Sci U S A</addtitle><date>2016-10-25</date><risdate>2016</risdate><volume>113</volume><issue>43</issue><spage>12071</spage><epage>12075</epage><pages>12071-12075</pages><issn>0027-8424</issn><eissn>1091-6490</eissn><abstract>Coastal flood hazard varies in response to changes in storm surge climatology and the sea level. Here we combine probabilistic projections of the sea level and storm surge climatology to estimate the temporal evolution of flood hazard. We find that New York City’s flood hazard has increased significantly over the past two centuries and is very likely to increase more sharply over the 21st century. Due to the effect of sea level rise, the return period of Hurricane Sandy’s flood height decreased by a factor of ∼3× from year 1800 to 2000 and is estimated to decrease by a further ∼4.4× from 2000 to 2100 under a moderate-emissions pathway. When potential storm climatology change over the 21st century is also accounted for, Sandy’s return period is estimated to decrease by ∼3× to 17× from 2000 to 2100.</abstract><cop>United States</cop><pub>National Academy of Sciences</pub><pmid>27790992</pmid><doi>10.1073/pnas.1604386113</doi><tpages>5</tpages><orcidid>https://orcid.org/0000-0002-5571-1606</orcidid><orcidid>https://orcid.org/0000-0003-4016-9428</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0027-8424 |
ispartof | Proceedings of the National Academy of Sciences - PNAS, 2016-10, Vol.113 (43), p.12071-12075 |
issn | 0027-8424 1091-6490 |
language | eng |
recordid | cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5087008 |
source | JSTOR Archive Collection A-Z Listing; PubMed Central; Alma/SFX Local Collection; Free Full-Text Journals in Chemistry |
subjects | Climate Floods Hazards Hurricanes Physical Sciences Sea level Tidal waves |
title | Hurricane Sandy’s flood frequency increasing from year 1800 to 2100 |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-01T02%3A43%3A48IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_pubme&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Hurricane%20Sandy%E2%80%99s%20flood%20frequency%20increasing%20from%20year%201800%20to%202100&rft.jtitle=Proceedings%20of%20the%20National%20Academy%20of%20Sciences%20-%20PNAS&rft.au=Lin,%20Ning&rft.date=2016-10-25&rft.volume=113&rft.issue=43&rft.spage=12071&rft.epage=12075&rft.pages=12071-12075&rft.issn=0027-8424&rft.eissn=1091-6490&rft_id=info:doi/10.1073/pnas.1604386113&rft_dat=%3Cjstor_pubme%3E26472203%3C/jstor_pubme%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1835926124&rft_id=info:pmid/27790992&rft_jstor_id=26472203&rfr_iscdi=true |