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	<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>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-435-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/435/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/435/2007/cpd-3-435-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/435/2007/cpd-3-435-2007.pdf</fulltext_pdf>
	<start_page>435</start_page>
	<end_page>467</end_page>
	<publication_date>2007-03-05</publication_date>
	<article_title content_type="html">New constraints on the gas age-ice age difference along the EPICA ice cores, 0&amp;ndash;50 kyr</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Loulergue</name>
			<email>loulergue@lgge.obs.ujf-grenoble.fr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Parrenin</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>T. Blunier</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J.-M. Barnola</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>R. Spahni</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>A. Schilt</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>G. Raisbeck</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>J. Chappellaz</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire de Glaciologie et de Géophysique de l&apos;Environnement (LGGE), CNRS, Université Joseph Fourier &amp;ndash; Grenoble, BP96 38402 Saint Martin d&apos;Heres Cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland</affiliation>
		<affiliation numeration="3" content_type="html">Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM), IN2P3-CNRS-Université de Paris-Sud, Bat 108, 91405 Orsay Cedex, France</affiliation>
	</affiliations>
	<abstract content_type="html">Gas is trapped in polar ice sheets at ~50&amp;ndash;120 m below the surface and
is therefore younger than the surrounding ice. Firn densification models are
used to evaluate this ice age-gas age difference (&amp;Delta;age) in the past.
However, such models are not well tested on low accumulation and cold sites
of the East Antarctic plateau, especially for periods with different
climatic conditions. Here we bring new constraints to test a firn
densification model applied to the EPICA Dome C (EDC) site for the last 50
kyr, by linking the EDC ice core to the EPICA Dronning Maud Land (EDML) ice
core, both in the ice phase (using volcanic horizons) and in the gas phase
(using rapid methane variations). We use the structured &lt;sup&gt;10&lt;/sup&gt;Be peak,
occurring 41 kyr before present (BP) and due to the low geomagnetic field
associated with the Laschamp event, to experimentally estimate the &amp;Delta;age and &amp;Delta;depth during this event. It allows us to evaluate the
model and to link together climatic archives from EDC and EDML to NorthGRIP
(Greenland). Our results reveal an overestimate of the &amp;Delta;age by the
firn densification model during the last glacial period at EDC. Tests with
different accumulation rates and temperature scenarios do not entirely
resolve this discrepancy. Our finding suggests that the phase relationship
between CO&lt;sub&gt;2&lt;/sub&gt; and EDC temperature inferred at the start of the last
deglaciation (lag of CO&lt;sub&gt;2&lt;/sub&gt; by 800&amp;plusmn;600 yr) is overestimated and
that the CO&lt;sub&gt;2&lt;/sub&gt; increase could well have been in phase or slightly leading
the temperature increase at EDC.</abstract>
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