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Variability in storm climate along the Gulf of Cadiz: the role of large scale atmospheric forcing and implications to coastal hazards

dc.contributor.authorPlomaritis, Theocharis
dc.contributor.authorBenavente, Javier
dc.contributor.authorLaiz, Irene
dc.contributor.authorDel Río, Laura
dc.date.accessioned2018-01-16T18:33:38Z
dc.date.available2018-01-16T18:33:38Z
dc.date.issued2015-11
dc.description.abstractIn the context of increased coastal hazards due to variability in storminess patterns, the danger of coastal damages and/or morphological changes is related to the sum of sea level conditions, storm surge, maximum wave height and run up values. In order to better understand the physical processes that cause the variability of the above parameters a 44 years reanalysis record (HIPOCAS) was used. The HIPOCAS time-series was validated with real wave and sea-level data using linear and vector correlation methods. In the present work changes in the magnitude, duration, frequency and approach direction of the Atlantic storms over the Gulf of Cadiz (SW Iberian Peninsula) were identified by computing various storm characteristics such as maximum wave height, total energy per storm wave direction and storm duration. The obtained time-series were compared with large-scale atmospheric indices such as the North Atlantic Oscillation (NAO) and the East Atlantic pattern. The results show a good correlation between negative NAO values and increased storminess over the entire Gulf of Cadiz. Furthermore, negative NAO values were correlated with high residual sea level values. Finally, a joint probability analysis of storm and sea level analysis resulted in increased probabilities of the two events happening at the same time indicating higher vulnerability of the coast and increased coastal risks. The above results were compared with coastal inundation events that took place over the last winter seasons in the province of Cadiz.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.1007/s00382-015-2486-4pt_PT
dc.identifier.issn0930-7575
dc.identifier.urihttp://hdl.handle.net/10400.1/10317
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherSpringer Verlagpt_PT
dc.relationResilience-Increasing Strategies for Coasts - toolKIT
dc.relationMorphological Impacts and COastal Risks induced by Extreme storm events
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectNAOpt_PT
dc.subjectEApt_PT
dc.subjectWave heightpt_PT
dc.subjectSea levelpt_PT
dc.subjectJoint probabilitypt_PT
dc.subjectStorm climatept_PT
dc.titleVariability in storm climate along the Gulf of Cadiz: the role of large scale atmospheric forcing and implications to coastal hazardspt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.awardTitleResilience-Increasing Strategies for Coasts - toolKIT
oaire.awardTitleMorphological Impacts and COastal Risks induced by Extreme storm events
oaire.awardURIinfo:eu-repo/grantAgreement/EC/FP7/603458/EU
oaire.awardURIinfo:eu-repo/grantAgreement/EC/FP7/202798/EU
oaire.citation.endPage2514pt_PT
oaire.citation.issue9-10pt_PT
oaire.citation.startPage2499pt_PT
oaire.citation.titleClimate Dynamicspt_PT
oaire.citation.volume45pt_PT
oaire.fundingStreamFP7
oaire.fundingStreamFP7
person.familyNamePlomaritis
person.givenNameTheocharis A.
person.identifier.ciencia-idFB1D-6248-EB10
person.identifier.orcid0000-0002-9819-0927
person.identifier.scopus-author-id22836553200
project.funder.identifierhttp://doi.org/10.13039/501100008530
project.funder.identifierhttp://doi.org/10.13039/501100008530
project.funder.nameEuropean Commission
project.funder.nameEuropean Commission
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication2937a782-dc45-4019-9dc3-7ad13f729c1c
relation.isAuthorOfPublication.latestForDiscovery2937a782-dc45-4019-9dc3-7ad13f729c1c
relation.isProjectOfPublication32d71a50-4c49-45ec-a98d-dee9226309ca
relation.isProjectOfPublication56278dca-1378-4880-a473-3927fbf9f956
relation.isProjectOfPublication.latestForDiscovery56278dca-1378-4880-a473-3927fbf9f956

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