Mostrar el registro sencillo del ítem

Surface circulation in Todos Santos Bay, Baja California, Mexico

dc.rights.licenseopenen_US
dc.contributor.authorDURAZO, Reginaldo
dc.contributor.authorFLORES-VIDAL, Xavier
dc.contributor.authorCASTRO, Ruben
hal.structure.identifierUniversidad Nacional Autónoma de México = National Autonomous University of Mexico [UNAM]
dc.contributor.authorOCAMPO-TORRES, Francisco J.
dc.contributor.authorSAAVEDRA, Johanna
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorRODRIGUEZ PADILLA, Isaac
hal.structure.identifierLaboratoire d'études en Géophysique et océanographie spatiales [LEGOS]
dc.contributor.authorLARRANAGA, Marco
dc.date.accessioned2025-03-31T09:15:10Z
dc.date.available2025-03-31T09:15:10Z
dc.date.issued2024-02
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/205810
dc.description.abstractEnDepending on dimensions, orientation and topographic features, the circulation of semi-enclosed seas adjacent to regions of coastal upwelling are strongly influenced by their interaction with a shelf upwelling jet of adjacent waters. A special case are square bays, where opening is about the same size as length, and are bordered by headlands at the entrance. This study analyzed surface currents measured between 2009 and 2020 with high-frequency (HF) radar in Todos Santos Bay, a square bay located in northwestern México, to obtain mean and seasonal surface circulation patterns. HF radar measurements indicate that the average circulation pattern within the bay is cyclonic, with water of the California Current (CC) entering primarily as a coastal jet through the northern mouth of the bay. The similarity of monthly average maps with the long-term average suggests the cyclonic circulation persists year-round. Scale analysis demonstrates that given the size of the bay, only one eddy, primarily controlled by inertia, is dominantly formed inside. The mean cyclonic circulation defines the bay as an upwelling shadow.
dc.language.isoENen_US
dc.title.enSurface circulation in Todos Santos Bay, Baja California, Mexico
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.csr.2024.105171en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terreen_US
bordeaux.journalCONTINENTAL SHELF RESEARCHen_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04720405
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=CONTINENTAL%20SHELF%20RESEARCH&rft.date=2024-02&rft.au=DURAZO,%20Reginaldo&FLORES-VIDAL,%20Xavier&CASTRO,%20Ruben&OCAMPO-TORRES,%20Francisco%20J.&SAAVEDRA,%20Johanna&rft.genre=article


Archivos en el ítem

ArchivosTamañoFormatoVer

No hay archivos asociados a este ítem.

Este ítem aparece en la(s) siguiente(s) colección(ones)

Mostrar el registro sencillo del ítem