A Process Study of the Wind-Induced Circulation in the Persian Gulf

Type Publication
Date 2013
Language English
Copyright 2013 SciRes.
Author(s) Pous Stephane1, Carton Xavier2, Lazure Pascal3
Affiliation(s) 1 : Université Pierre et Marie Curie, Paris, France
2 : Université de Bretagne Occidentale, Brest, France
3 : Ifremer, Brest, France
Source Open Journal of Marine Science (2161-7384) (Scientific Research Publishing, Inc,), 2013 , Vol. 03 , N. 01 , P. 1-11
DOI 10.4236/ojms.2013.31001
Keyword(s) Persian Gulf, Wind-Induced Circulation, Hydrodynamical Modeling
Abstract A shallow-water model, coupled with a three dimensional, hydrostatic ocean model, is used to study the wind induced circulation, and the Shatt-al-Arab river plume expansion, in the Persian Gulf. The models are used in an idealized configuration. The following results are obtained: 1) with northwesterly winds, a double gyre is formed: this gyre is cyclonic in the south and anticyclonic in the north. Southeastward currents flow along the Iranian and Arabian coast where the wind stress at the surface dominates the pressure gradient related to the free surface slope, and conversely in the deeper region of the Gulf; 2) In the eastern part of the Gulf, the cyclonic gyre intensifies, as observed and reported in the literature; 3) For northwesterly winds, the plume from Shatt-al-Arab first heads towards the Iranian coast and then spreads southeastward along the Arabian coast; for northerly and northeasterly winds, the plume directly follows the Kuwaiti coast and then the Arabian coast. This sensitivity of the orientation can be related to the double gyre flow structure; 4) A southeasterly wind confines the plume in the northern end of the Gulf as does a pure tidal flow.
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