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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>3</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cp-3-541-2007</doi>
	<article_url>http://www.clim-past.net/3/541/2007/</article_url>
	<abstract_html>http://www.clim-past.net/3/541/2007/cp-3-541-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/3/541/2007/cp-3-541-2007.pdf</fulltext_pdf>
	<start_page>541</start_page>
	<end_page>547</end_page>
	<publication_date>2007-09-07</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">Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse, IN2P3-CNRS-Université de Paris-Sud, Bât. 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, 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 this time period, 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 observed between A1 and A2.</abstract>
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</article>

