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Ocean Science An interactive open-access journal of the European Geosciences Union
Ocean Sci., 2, 27-41, 2006
https://doi.org/10.5194/os-2-27-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
 
05 Jul 2006
The circulation of the Persian Gulf: a numerical study
J. Kämpf1 and M. Sadrinasab2 1School of Chemistry, Physics and Earth Sciences, Flinders Research Centre for Coast and Catchment Environments, Flinders University, Adelaide, Australia
2Khorramshahr University of Nautical Sciences & Technology, Khorramshahr, Iran
Abstract. 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.

Citation: Kämpf, J. and Sadrinasab, M.: The circulation of the Persian Gulf: a numerical study, Ocean Sci., 2, 27-41, https://doi.org/10.5194/os-2-27-2006, 2006.
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