Increased extreme coastal water levels due to the combined action of storm surges and wind waves
The dependence between extreme storm surges and wind waves is assessed statistically along the global coasts using the outputs of two numerical models consistently forced with the same atmospheric fields. We show that 55% of the world coastlines face compound storm surge wave extremes. Hence, for a...
| Autores: | , , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2019 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/202987 |
| Acceso en línea: | http://hdl.handle.net/10261/202987 |
| Access Level: | acceso abierto |
| Palabra clave: | sea level extremes storm surges wind waves compound events Coastal flooding |
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Increased extreme coastal water levels due to the combined action of storm surges and wind wavesMarcos, MartaRohmer, JérémyVousdoukas, Michalis I.Mentaschi, LorenzoCozannet, GonériAmores, Ángelsea level extremesstorm surgeswind wavescompound eventsCoastal floodingThe dependence between extreme storm surges and wind waves is assessed statistically along the global coasts using the outputs of two numerical models consistently forced with the same atmospheric fields. We show that 55% of the world coastlines face compound storm surge wave extremes. Hence, for a given level of probability, neglecting these dependencies leads to underestimating extreme coastal water levels. Dependencies are dominant in midlatitudes and are likely underestimated in the tropics due to limited representation of tropical cyclones. Furthermore, we show that in half of the areas with dependence, the estimated probability of occurrence of coastal extreme water levels increases significantly when it is accounted for. Translated in terms of return periods, this means that along 30% of global coastlines, extreme water levels expected at most once in a century without considering dependence between storm surges and waves become a 1 in 50-year event.This study was supported by the ERA4CS INSeaPTION project (grants 690462 and PCIN‐2017‐038).John Wiley & SonsEuropean CommissionMinisterio de Ciencia, Innovación y Universidades (España)Agencia Estatal de Investigación (España)Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]2020202020192020info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionhttp://hdl.handle.net/10261/202987reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/EC/H2020/690462info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PCIN-2017-038PCIN-2017-038/AEI/10.13039/501100011033http://doi.org/10.1029/2019GL082599Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/2029872026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves |
| title |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves |
| spellingShingle |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves Marcos, Marta sea level extremes storm surges wind waves compound events Coastal flooding |
| title_short |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves |
| title_full |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves |
| title_fullStr |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves |
| title_full_unstemmed |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves |
| title_sort |
Increased extreme coastal water levels due to the combined action of storm surges and wind waves |
| dc.creator.none.fl_str_mv |
Marcos, Marta Rohmer, Jérémy Vousdoukas, Michalis I. Mentaschi, Lorenzo Cozannet, Gonéri Amores, Ángel |
| author |
Marcos, Marta |
| author_facet |
Marcos, Marta Rohmer, Jérémy Vousdoukas, Michalis I. Mentaschi, Lorenzo Cozannet, Gonéri Amores, Ángel |
| author_role |
author |
| author2 |
Rohmer, Jérémy Vousdoukas, Michalis I. Mentaschi, Lorenzo Cozannet, Gonéri Amores, Ángel |
| author2_role |
author author author author author |
| dc.contributor.none.fl_str_mv |
European Commission Ministerio de Ciencia, Innovación y Universidades (España) Agencia Estatal de Investigación (España) Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
sea level extremes storm surges wind waves compound events Coastal flooding |
| topic |
sea level extremes storm surges wind waves compound events Coastal flooding |
| description |
The dependence between extreme storm surges and wind waves is assessed statistically along the global coasts using the outputs of two numerical models consistently forced with the same atmospheric fields. We show that 55% of the world coastlines face compound storm surge wave extremes. Hence, for a given level of probability, neglecting these dependencies leads to underestimating extreme coastal water levels. Dependencies are dominant in midlatitudes and are likely underestimated in the tropics due to limited representation of tropical cyclones. Furthermore, we show that in half of the areas with dependence, the estimated probability of occurrence of coastal extreme water levels increases significantly when it is accounted for. Translated in terms of return periods, this means that along 30% of global coastlines, extreme water levels expected at most once in a century without considering dependence between storm surges and waves become a 1 in 50-year event. |
| publishDate |
2019 |
| dc.date.none.fl_str_mv |
2019 2020 2020 2020 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Publisher's version info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/202987 |
| url |
http://hdl.handle.net/10261/202987 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
#PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/H2020/690462 info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PCIN-2017-038 PCIN-2017-038/AEI/10.13039/501100011033 http://doi.org/10.1029/2019GL082599 Sí |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
John Wiley & Sons |
| publisher.none.fl_str_mv |
John Wiley & Sons |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
| instname_str |
Consejo Superior de Investigaciones Científicas (CSIC) |
| reponame_str |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
| collection |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
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| repository.mail.fl_str_mv |
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1869425163131420672 |
| score |
15,81155 |