Afficher la notice abrégée

dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCASTELLE, Bruno
IDREF: 087596520
hal.structure.identifierLittoral, Environnement, Télédétection, Géomatique [LETG - Brest]
dc.contributor.authorDODET, Guillaume
hal.structure.identifierPlymouth University
dc.contributor.authorMASSELINK, Gerd
hal.structure.identifierPlymouth University
dc.contributor.authorSCOTT, Tim
dc.date.accessioned2024-04-18T07:53:57Z
dc.date.available2024-04-18T07:53:57Z
dc.date.issued2017-02-16
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199213
dc.description.abstractEnA pioneering and replicable method based on a 66-year numerical weather and wave hindcast is developed to optimize a climate index based on the sea level pressure (SLP) that best explains winter wave height variability along the coast of western Europe, from Portugal to UK (36–52 ∘ N). The resulting so-called Western Europe Pressure Anomaly (WEPA) is based on the sea level pressure gradient between the stations Valentia (Ireland) and Santa Cruz de Tenerife (Canary Islands). The WEPA positive phase reflects an intensified and southward shifted SLP difference between the Icelandic low and the Azores high, driving severe storms that funnel high-energy waves toward western Europe southward of 52 ∘ N. WEPA outscores by 25–150% the other leading atmospheric modes in explaining winter-averaged significant wave height, and even by a largest amount the winter-averaged extreme wave heights. WEPA is also the only index capturing the 2013/2014 extreme winter that caused widespread coastal erosion and flooding in western Europe.
dc.description.sponsorshipLabexMER Marine Excellence Research: a changing ocean - ANR-10-LABX-0019en_US
dc.description.sponsorshipProcessus cross-shore et longshore combinés en morphodynamique littorale - ANR-14-ASTR-0004en_US
dc.language.isoENen_US
dc.title.enA new climate index controlling winter wave activity along the Atlantic coast of Europe: The West Europe Pressure Anomaly
dc.typeArticle de revueen_US
dc.identifier.doi10.1002/2016GL072379en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographieen_US
bordeaux.journalGeophysical Research Lettersen_US
bordeaux.page1384 - 1392en_US
bordeaux.volume44en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue3en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01598309
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geophysical%20Research%20Letters&rft.date=2017-02-16&rft.volume=44&rft.issue=3&rft.spage=1384%20-%201392&rft.epage=1384%20-%201392&rft.eissn=0094-8276&rft.issn=0094-8276&rft.au=CASTELLE,%20Bruno&DODET,%20Guillaume&MASSELINK,%20Gerd&SCOTT,%20Tim&rft.genre=article


Fichier(s) constituant ce document

Thumbnail

Ce document figure dans la(les) collection(s) suivante(s)

Afficher la notice abrégée