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dc.contributor.authorMosaddad, Seyed Majid-
dc.contributor.authorDelphi, Mehdi-
dc.date.accessioned2014-03-03T06:40:46Z-
dc.date.available2014-03-03T06:40:46Z-
dc.date.issued2014-02-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/27261-
dc.description252-257en_US
dc.description.abstractIn the present study, authors present evidence of a clear coupling between thermocline and turbulence in northern part of the Persian Gulf (PG). A mechanism for generating the turbulence observed on the thermocline sheets is established by running a turbulence closure through the POM (Princeton Ocean Model), established by1. Turbulence kinetic energy increasing will be resulted from winter to summer due to thermocline development in northern part of the PG.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.43(2) [February 2014]en_US
dc.subjectPersian gulfen_US
dc.subjectPrinceton ocean modelen_US
dc.subjectTurbulenceen_US
dc.titleNumerical simulation of turbulence in Northern part of the Persian Gulfen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.43(02) [February 2014]

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