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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>4</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-999-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/999/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/999/2007/cpd-3-999-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/999/2007/cpd-3-999-2007.pdf</fulltext_pdf>
	<start_page>999</start_page>
	<end_page>1020</end_page>
	<publication_date>2007-08-24</publication_date>
	<article_title content_type="html">Information on the early Holocene climate constrains the summer sea ice projections for the 21st century</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Goosse</name>
			<email>hgs@astr.ucl.ac.be</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>E. Driesschaert</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. Fichefet</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>M.-F. Loutre</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Université Catholique de Louvain, Institut d&apos;Astronomie et de Géophysique G. Lemaître, Chemin du Cyclotron, 2, 1348 Louvain-la-Neuve, Belgium</affiliation>
	</affiliations>
	<abstract content_type="html">The summer sea ice extent strongly decreased in the Arctic over the last
decades. This decline is very likely to continue in the future but
uncertainty on projections is very large. An ensemble of experiments with
the climate model LOVECLIM using 5 different parameter sets has been
performed to show that summer sea ice changes for the early Holocene and for
the 21st century are strongly linked, allowing to reduce this
uncertainty. Using the limited information presently available for the early
Holocene, simulations presenting very large changes for the 21st
century could reasonably be rejected. On the other hand, simulations
displaying low to moderate changes during the second half of the 20th
century are not consistent with recent observations. Using this evidence
based on observations during both the early Holocene and the last decades,
the most realistic projection indicates a nearly disappearance of the sea
ice at the end of the 21st century for a moderate increase in
atmospheric greenhouse gas concentrations. For a faster increase in those
concentrations, the Arctic Ocean would become almost ice-free in summer as
early as 2060 AD.</abstract>
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