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	<journal>
		<journal_title>Climate of the Past</journal_title>
		<journal_url>www.clim-past.net</journal_url>
		<issn>1814-9324</issn>
		<eissn>1814-9332</eissn>
		<volume_number>7</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2011</publication_year>
	</journal>
	<doi>10.5194/cp-7-339-2011</doi>
	<article_url>http://www.clim-past.net/7/339/2011/</article_url>
	<abstract_html>http://www.clim-past.net/7/339/2011/cp-7-339-2011.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/7/339/2011/cp-7-339-2011.pdf</fulltext_pdf>
	<start_page>339</start_page>
	<end_page>347</end_page>
	<publication_date>2011-04-04</publication_date>
	<article_title content_type="html">Solar-forced shifts of the Southern Hemisphere Westerlies during the Holocene</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. Varma</name>
			<email>vvarma@marum.de</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>M. Prange</name>
		</author>
		<author numeration="3" affiliations="2,3">
			<name>F. Lamy</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>U. Merkel</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>M. Schulz</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geosciences, University of Bremen, 28334 Bremen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Alfred Wegener Institute for Polar and Marine Research, 27568 Bremerhaven, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The Southern Hemisphere Westerly Winds (SWW) constitute an important zonal
circulation that influences large-scale precipitation patterns and ocean
circulation. Variations in their intensity and latitudinal position have
been suggested to exert a strong influence on the CO&lt;sub&gt;2&lt;/sub&gt; budget in the
Southern Ocean, thus making them a potential factor affecting the global
climate. In the present study, the possible influence of solar forcing on
SWW variability during the Holocene is addressed. It is shown that a
high-resolution iron record from the Chilean continental slope (41° S),
which is interpreted to reflect changes in the position of the SWW, is
significantly correlated with reconstructed solar activity during the past
3000 years. In addition, solar sensitivity experiments with a comprehensive
global climate model (CCSM3) were carried out to study the response of SWW to
solar variability. Taken together, the proxy and model results suggest that
centennial-scale periods of lower (higher) solar activity caused equatorward
(southward) shifts of the annual mean SWW.</abstract>
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</article>

