Sea surface temperature and Ekman transport in the Persian Gulf

The wind drift motion of the water which is produced by the stress of the wind exerted upon the surface of the ocean is described by Ekmans theory (1905). Using the mean monthly values for the wind stress and SST, seasonal Ekman transport for the Persian Gulf was computed and contoured. The geostrop...

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Main Authors: E. H., H. N.
Format: Article
Language:English
Published: Isfahan University of Technology 2002-12-01
Series:Iranian Journal of Physics Research
Subjects:
Online Access:http://ijpr.iut.ac.ir/browse.php?a_code=A-10-1-238&slc_lang=en&sid=1
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author E. H.
H. N.
author_facet E. H.
H. N.
author_sort E. H.
collection DOAJ
description The wind drift motion of the water which is produced by the stress of the wind exerted upon the surface of the ocean is described by Ekmans theory (1905). Using the mean monthly values for the wind stress and SST, seasonal Ekman transport for the Persian Gulf was computed and contoured. The geostrophic winds have combined with the SST to estimate the effect of cooling due to Ekman transport of colder northern waters and inflow from the Oman Sea. The monthly SST mainly obtained from the 10 10 grided data of Levitus atlas and Hormuz Cruis Experiment for 1997.   Analyses show a NW to SE Ekman transport due to wind stress and significant interannual variability of SST on sea surface in the Persian Gulf. The seasonal variation of SST shows a continental pattern due to severe interaction between the land and sea. But these variations somehow moderates because of Ekman transport in Persian Gulf.
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spelling doaj.art-09b18bd2513649069afb37507fa7843d2022-12-22T03:19:17ZengIsfahan University of TechnologyIranian Journal of Physics Research1682-69572002-12-0133213222Sea surface temperature and Ekman transport in the Persian GulfE. H.H. N.The wind drift motion of the water which is produced by the stress of the wind exerted upon the surface of the ocean is described by Ekmans theory (1905). Using the mean monthly values for the wind stress and SST, seasonal Ekman transport for the Persian Gulf was computed and contoured. The geostrophic winds have combined with the SST to estimate the effect of cooling due to Ekman transport of colder northern waters and inflow from the Oman Sea. The monthly SST mainly obtained from the 10 10 grided data of Levitus atlas and Hormuz Cruis Experiment for 1997.   Analyses show a NW to SE Ekman transport due to wind stress and significant interannual variability of SST on sea surface in the Persian Gulf. The seasonal variation of SST shows a continental pattern due to severe interaction between the land and sea. But these variations somehow moderates because of Ekman transport in Persian Gulf.http://ijpr.iut.ac.ir/browse.php?a_code=A-10-1-238&slc_lang=en&sid=1sea surface temperaturesalinitythermohalineEkman transportPersian Gulf
spellingShingle E. H.
H. N.
Sea surface temperature and Ekman transport in the Persian Gulf
Iranian Journal of Physics Research
sea surface temperature
salinity
thermohaline
Ekman transport
Persian Gulf
title Sea surface temperature and Ekman transport in the Persian Gulf
title_full Sea surface temperature and Ekman transport in the Persian Gulf
title_fullStr Sea surface temperature and Ekman transport in the Persian Gulf
title_full_unstemmed Sea surface temperature and Ekman transport in the Persian Gulf
title_short Sea surface temperature and Ekman transport in the Persian Gulf
title_sort sea surface temperature and ekman transport in the persian gulf
topic sea surface temperature
salinity
thermohaline
Ekman transport
Persian Gulf
url http://ijpr.iut.ac.ir/browse.php?a_code=A-10-1-238&slc_lang=en&sid=1
work_keys_str_mv AT eh seasurfacetemperatureandekmantransportinthepersiangulf
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