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Titel The circulation of the Persian Gulf: a numerical study
VerfasserIn J. Kämpf, M. Sadrinasab
Medientyp Artikel
Sprache Englisch
ISSN 1812-0784
Digitales Dokument URL
Erschienen In: Ocean Science ; 2, no. 1 ; Nr. 2, no. 1 (2006-07-05), S.27-41
Datensatznummer 250000404
Publikation (Nr.) Volltext-Dokument vorhandencopernicus.org/os-2-27-2006.pdf
 
Zusammenfassung
We employ a three-dimensional hydrodynamic model (COHERENS) in a fully prognostic mode to study the circulation and water mass properties of the Persian Gulf – a large inverse estuary. Our findings, which are in good agreement with observational evidence, suggest that the Persian Gulf experiences a distinct seasonal cycle in which a gulf-wide cyclonic overturning circulation establishes in spring and summer, but this disintegrates into mesoscale eddies in autumn and winter. Establishment of the gulf-wide circulation coincides with establishment of thermal stratification and strengthening of the baroclinic exchange circulation through the Strait of Hormuz. Winter cooling of extreme saline (>45) water in shallow regions along the coast of United Arab Emirates is a major driver of this baroclinic circulation.
 
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