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<!DOCTYPE article SYSTEM "http://www.clim-past-discuss.net/inc/cpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>2</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/cpd-2-605-2006</doi>
	<article_url>http://www.clim-past-discuss.net/2/605/2006/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/2/605/2006/cpd-2-605-2006.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/2/605/2006/cpd-2-605-2006.pdf</fulltext_pdf>
	<start_page>605</start_page>
	<end_page>631</end_page>
	<publication_date>2006-08-23</publication_date>
	<article_title content_type="html">Effect of vegetation on the Late Miocene ocean circulation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Lohmann</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. Butzin</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>A. Micheels</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>T. Bickert</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>V. Mosbrugger</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Alfred-Wegener-Institut für Polar- und Meeresforschung, Bussestr. 24, 27570 Bremerhaven, Germany</affiliation>
		<affiliation numeration="2" content_type="html">University of Bremen, P.O. Box 330440, 28334 Bremen, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Senckenberg Research Institute and Natural History Museum, Senckenberganlage 25, 60325 Frankfurt am Main, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">A weak and shallow thermohaline circulation in the North Atlantic Ocean is
related to an open Central American gateway and exchange with fresh Pacific
waters. We estimate the effect of vegetation on the ocean general
circulation using the atmospheric circulation model simulations for the Late
Miocene climate. Caused by an increase in net evaporation in the Miocene
North Atlantic, the North Atlantic water becomes more saline which enhances
the overturning circulation and thus the northward heat transport. This
effect reveals a potentially important feedback between the ocean
circulation, the hydrological cycle and the land surface cover for Cenozoic
climate evolution.</abstract>
	<references>
	</references>
</article>

