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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>3</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-755-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/755/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/755/2007/cpd-3-755-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/755/2007/cpd-3-755-2007.pdf</fulltext_pdf>
	<start_page>755</start_page>
	<end_page>769</end_page>
	<publication_date>2007-05-11</publication_date>
	<article_title content_type="html">Direct North-South synchronization of abrupt climate change record in ice cores using beryllium 10</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. M. Raisbeck</name>
			<email>raisbeck@csnsm.in2p3.fr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Yiou</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J. Jouzel</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>T. F. Stocker</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CSNSM/IN2P3/CNRS, Bat 108, 91405 Orsay, France</affiliation>
		<affiliation numeration="2" content_type="html">IPSL/LSCE, UMR CEA-CNRS-UVSQ, CE Saclay, 91191 Gif-sur-Yvette, France</affiliation>
		<affiliation numeration="3" content_type="html">Climate and Environmental Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">A new, decadally resolved record of the &lt;sup&gt;10&lt;/sup&gt;Be peak at 41 kyr from the
EPICA Dome C ice core (Antarctica) is used to match it with the same peak in
the GRIP ice core (Greenland). This permits a direct synchronisation of the
climatic variations around 41 kyr BP, independent of uncertainties related
to the ice age-gas age difference in ice cores. Dansgaard-Oeschger event 10
is in the period of best synchronisation and is found to be coeval with an
Antarctic temperature maximum. Simulations using a thermal bipolar seesaw
model agree reasonably well with the observed relative climate chronology in
these two cores. They also reproduce three Antarctic warming events between
A1 and A2.</abstract>
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</article>

