Publication:
Wave storm events in the western mediterranean sea over four decades

dc.contributor.authorAmarouche, Khalid
dc.contributor.authorAkpınar, Adem
dc.contributor.authorSemedo, Alvaro
dc.contributor.buuauthorAMAROUCHE, KHALID
dc.contributor.buuauthorAKPINAR, ADEM
dc.contributor.departmentBursa Uludağ Üniversitesi/Mühendislik Fakültesi/İnşaat Mühendisliği Bölümü
dc.contributor.orcid0000-0001-7983-4611
dc.contributor.researcheridAAC-6763-2019
dc.contributor.researcheridAFR-7886-2022
dc.date.accessioned2024-10-14T06:55:59Z
dc.date.available2024-10-14T06:55:59Z
dc.date.issued2022-01-14
dc.description.abstractThe rising intensity and recurrence of wave storm events can seriously impact navigation and coastal and offshore structures in the Western Mediterranean Sea. Therefore, the present study is focused on wave storm events in the Western Mediterranean Sea, over the last four decades. The spatial decadal variations of wave storm events are shown, considering variations in the parameters that characterise wave storms, such as significant wave height (SWH), wave storm duration, and wave storm direction. Additionally, the decadal variation in wave storm intensities is evaluated through the storm power index (SPI) and the total storm wave energy (TSWE). The study is based on a wave hindcast, developed using a calibrated SWAN model. The wave storm events are obtained based on the SWH time series for 24 325 locations, distributed over an unstructured grid, covering the entire Western Mediterranean Sea. The decadal variation in the number of wave storm events, maximum and mean wave storm duration, SPI, and TSWE were observed in large parts of the West Mediterranean Sea during the last four decades. However, variations in mean SWH during these storms are low, and do not show a real implication in the decadal changes in the wave storm intensity (SPI and TSWE). Locations of significant increasing changes in SPI and TSWE show a dependence on changes in the wave storm duration. They may be related to variations in wave storm direction in some areas. Increases in wave storm duration are mainly responsible for increases in wave storm intensities over the last decade.
dc.identifier.doi10.1016/j.ocemod.2021.101933
dc.identifier.eissn1463-5011
dc.identifier.issn1463-5003
dc.identifier.urihttps://doi.org/10.1016/j.ocemod.2021.101933
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S1463500321001815
dc.identifier.urihttps://hdl.handle.net/11452/46338
dc.identifier.volume170
dc.identifier.wos000787885400004
dc.indexed.wosWOS.SCI
dc.language.isoen
dc.publisherElsevier
dc.relation.journalOcean Modelling
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectClimate-change
dc.subjectRegional-scale
dc.subjectSurface temperature
dc.subjectNumerical-models
dc.subjectMesh generation
dc.subjectCoastal regions
dc.subjectGlobal trends
dc.subjectWind-speed
dc.subjectVariability
dc.subjectSwan
dc.subjectWave storms
dc.subjectDecadal variations
dc.subjectWind waves
dc.subjectWave storm durations
dc.subjectWestern mediterranean sea
dc.subjectScience & technology
dc.subjectPhysical sciences
dc.subjectMeteorology & atmospheric sciences
dc.subjectOceanography
dc.titleWave storm events in the western mediterranean sea over four decades
dc.typeArticle
dspace.entity.typePublication
relation.isAuthorOfPublicationb281fc06-da71-4666-bb0c-33292bc43ec8
relation.isAuthorOfPublication7613a1fe-c70a-4b3c-9424-e4d5cabe5d81
relation.isAuthorOfPublication.latestForDiscoveryb281fc06-da71-4666-bb0c-33292bc43ec8

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