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Study of Internal Waves in the Persian Gulf
The Persian Gulf (PG), as a semi-enclosed water basin extends in (47-57) E, (24-30) N, geographic domain. Particularly, northern part of the PG shows more baroclinicity and turbulence because of the river inflow from the Arvand, bottom and costal stresses. Furthermore, wind stress has many effects rather than in mid deep domain of the PG. Thermocli... Read More»
: J Marine Sci Res Dev
10.4172/2155-9910.1000276Abstract Peer-reviewed Full Article Peer-reviewed Article PDF Mobile Full Article
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