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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>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-19-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/19/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/19/2007/cpd-3-19-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/19/2007/cpd-3-19-2007.pdf</fulltext_pdf>
	<start_page>19</start_page>
	<end_page>61</end_page>
	<publication_date>2007-01-16</publication_date>
	<article_title content_type="html">Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>F. Parrenin</name>
			<email>parrenin@ujf-grenoble.fr</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>G. Dreyfus</name>
		</author>
		<author numeration="3" affiliations="1,3">
			<name>G. Durand</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>S. Fujita</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>O. Gagliardini</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>F. Gillet</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>J. Jouzel</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>K. Kawamura</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>N. Lhomme</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>V. Masson-Delmotte</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>C. Ritz</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>J. Schwander</name>
		</author>
		<author numeration="13" affiliations="7">
			<name>H. Shoji</name>
		</author>
		<author numeration="14" affiliations="4">
			<name>R. Uemura</name>
		</author>
		<author numeration="15" affiliations="4">
			<name>O. Watanabe</name>
		</author>
		<author numeration="16" affiliations="8">
			<name>N. Yoshida</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire de Glaciologie et Géophysique de l&apos;Environnement, CNRS and Joseph Fourier University, Grenoble, France</affiliation>
		<affiliation numeration="2" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environnement, Gif-Sur-Yvette, France</affiliation>
		<affiliation numeration="3" content_type="html">Niels Bohr Institute for Astronomy, Physics and Geophysics, Copenhagen, Denmark</affiliation>
		<affiliation numeration="4" content_type="html">National Institute of Polar Research, Research Organization of Information and Systems (ROIS), Tokyo, Japan</affiliation>
		<affiliation numeration="5" content_type="html">Center for Atmospheric and Oceanic Studies Graduate School of Science, Tohoku University, Sendai, Japan</affiliation>
		<affiliation numeration="6" content_type="html">Physics Institute, University of Bern, Switzerland</affiliation>
		<affiliation numeration="7" content_type="html">New Energy Resources Research Center, Kitami Institute of Technology, Kitami, Japan</affiliation>
		<affiliation numeration="8" content_type="html">Frontier Collaborative Research Center, Yokohama, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">1-D ice flow models are used to construct the age scales at the Dome C and
Dome Fuji drilling sites (East Antarctica). The poorly constrained
glaciological parameters at each site are recovered by fitting independent
age markers identified on each core. We reconstruct past accumulation rates,
that are larger than those modelled using the classical vapour saturation
pressure relationship during glacial periods by up to a factor 1.5. During
the Early Holocene, changes in reconstructed accumulation are not linearly
related to changes in ice
isotopic composition. A simple model of past elevation changes is developed
and shows an
amplitude variation of 110&amp;ndash;120 m at both sites. We suggest that there is
basal melting at Dome C (0.56&amp;plusmn;0.19 mm/yr). The reconstructed velocity
profile is highly non linear at both sites, which suggests complex ice flow
effects. This induces a non linear thinning function in both drilling sites,
which is also characterized by bumps corresponding to variations in surface
elevation with time.</abstract>
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</article>

