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<article language="en">
	<journal>
		<journal_title>Ocean Science</journal_title>
		<journal_url>www.ocean-sci.net</journal_url>
		<issn>1812-0784</issn>
		<eissn>1812-0792</eissn>
		<volume_number>2</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/os-2-27-2006</doi>
	<article_url>http://www.ocean-sci.net/2/27/2006/</article_url>
	<abstract_html>http://www.ocean-sci.net/2/27/2006/os-2-27-2006.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/2/27/2006/os-2-27-2006.pdf</fulltext_pdf>
	<start_page>27</start_page>
	<end_page>41</end_page>
	<publication_date>2006-07-05</publication_date>
	<article_title content_type="html">The circulation of the Persian Gulf: a numerical study</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Kämpf</name>
			<email>jochen.kaempf@flinders.edu.au</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. Sadrinasab</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Chemistry, Physics and Earth Sciences, Flinders Research  Centre for Coast and Catchment Environments, Flinders University, Adelaide,  Australia</affiliation>
		<affiliation numeration="2" content_type="html">Khorramshahr University of Nautical Sciences &amp; Technology, Khorramshahr, Iran</affiliation>
	</affiliations>
	<abstract content_type="html">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 &amp;ndash; 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 (&gt;45) water
in shallow regions along the coast of United Arab Emirates is a major driver
of this baroclinic circulation.</abstract>
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</article>

