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<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>6</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/cpd-6-19-2010</doi>
	<article_url>http://www.clim-past-discuss.net/6/19/2010/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/6/19/2010/cpd-6-19-2010.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/6/19/2010/cpd-6-19-2010.pdf</fulltext_pdf>
	<start_page>19</start_page>
	<end_page>34</end_page>
	<publication_date>2010-01-29</publication_date>
	<article_title content_type="html">Patterns of millennial variability over the last 500 ka</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Siddall</name>
			<email>mark.siddall@bristol.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>E. J. Rohling</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>T. Blunier</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>R. Spahni</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth Science, University of Bristol, Bristol, UK</affiliation>
		<affiliation numeration="2" content_type="html">National Oceanography Centre, Southampton, Southampton, UK</affiliation>
		<affiliation numeration="3" content_type="html">Centre for Ice &amp; Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark</affiliation>
		<affiliation numeration="4" content_type="html">Climate and Environmental Physics and Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">Millennial variability is a robust feature of many
      paleoclimate records, at least throughout the last several
      glacial cycles. Here we use the signal from an Antarctic
      climate event to probe the EPICA Dome C temperature proxy
      reconstruction through the last 500 ka for similar
      millennial-scale events. We find that clusters of millennial
      events occurred in a regular fashion over half of the time
      during this with a mean recurrence interval of 21 kyr. We
      find that there is no consistent link between ice-rafted
      debris deposition and millennial variability. Instead we
      speculate that changes in the zonality of atmospheric
      circulation over the North Atlantic form a viable alternative
      to freshwater release from icebergs as a trigger for
      millennial variability. We suggest that millennial changes in
      the zonality of atmospheric circulation over the North
      Atlantic are linked to precession and that this relationship
      is modified by the presence of the large, Northern Hemisphere
      ice sheets during glacial periods.</abstract>
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