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Simulating storm surge and compound flooding events with a creek-to-ocean model: Importance of baroclinic effects

dc.rights.licenseopenen_US
dc.contributor.authorYE, Fei
dc.contributor.authorZHANG, Yinglong J.
dc.contributor.authorYU, Haocheng
dc.contributor.authorSUN, Weiling
dc.contributor.authorMOGHIMI, Saeed
dc.contributor.authorMYERS, Edward
dc.contributor.authorNUNEZ, Karinna
dc.contributor.authorZHANG, Ruoyin
dc.contributor.authorWANG, Harry V.
dc.contributor.authorROLAND, Aron
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARTINS, Kevin
dc.contributor.authorBERTIN, Xavier
dc.contributor.authorDU, Jiabi
dc.contributor.authorLIU, Zhuo
dc.date.accessioned2024-02-05T16:24:22Z
dc.date.available2024-02-05T16:24:22Z
dc.date.issued2020-01-01
dc.identifier.issn1463-5003en_US
dc.identifier.urioai:crossref.org:10.1016/j.ocemod.2019.101526
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187844
dc.description.abstractEnWe present a creek-to-ocean 3D baroclinic model based on unstructured grids that aims to unite traditional hydrologic and ocean models in a single modeling platform, by taking full advantage of the polymorphism (i.e. a single model grid can seamlessly morph between full 3D, 2DV, 2DH and quasi-1D configurations). Using Hurricane Irene (2011)’s impact on the Delaware Bay as an example, a seamless 2D–3D model grid is implemented to include the entire US East Coast and Gulf of Mexico with a highly resolved Delaware Bay (down to 20-m resolution). The model is forced by flows from a hydrological model (National Water Model ) at the landward boundary. We demonstrate the model’s accuracy, stability and robustness with the simulation of the storm surge and subsequent river flooding events and compound surges. Through a series of sensitivity tests, we illustrate the importance of including in the simulation the baroclinic effects, as provided by the large-scale Gulf Stream, in order to correctly capture the adjustment process following the main surge and the subsequent compound flooding events. The baroclinicity can explain up to 14% of the elevation error during the adjustment phase after the storm.
dc.language.isoENen_US
dc.sourcecrossref
dc.title.enSimulating storm surge and compound flooding events with a creek-to-ocean model: Importance of baroclinic effects
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.ocemod.2019.101526en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalOcean Modellingen_US
bordeaux.page101526en_US
bordeaux.volume145en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04439865
hal.version1
hal.date.transferred2024-02-05T16:24:27Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Ocean%20Modelling&rft.date=2020-01-01&rft.volume=145&rft.spage=101526&rft.epage=101526&rft.eissn=1463-5003&rft.issn=1463-5003&rft.au=YE,%20Fei&ZHANG,%20Yinglong%20J.&YU,%20Haocheng&SUN,%20Weiling&MOGHIMI,%20Saeed&rft.genre=article


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