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<article language="en">
	<journal>
		<journal_title>The Cryosphere Discussions</journal_title>
		<journal_url>www.the-cryosphere-discuss.net</journal_url>
		<issn>1994-0432</issn>
		<eissn>1994-0440</eissn>
		<volume_number>1</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/tcd-1-351-2007</doi>
	<article_url>http://www.the-cryosphere-discuss.net/1/351/2007/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/1/351/2007/tcd-1-351-2007.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/1/351/2007/tcd-1-351-2007.pdf</fulltext_pdf>
	<start_page>351</start_page>
	<end_page>383</end_page>
	<publication_date>2007-09-10</publication_date>
	<article_title content_type="html">High-resolution simulations of the surface mass balance of Greenland at the end of this century</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Krinner</name>
			<email>krinner@ujf-grenoble.fr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>N. Julien</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">LGGE/CNRS-UJF Grenoble, France</affiliation>
	</affiliations>
	<abstract content_type="html">We present atmospheric general circulation model simulations of the present
(1981&amp;ndash;2005) and future (2081&amp;ndash;2100) climate according to the SRES A1B
greenhouse gas scenario. Focusing on Greenland, we use a stretched grid in
the global model, thereby reaching a horizontal grid spacing of 60 km in the
region of interest. This allows to capture reasonably the escarpment zone of
the ice sheet. For the end of this century, the model suggests a
precipitation increase in the central region of Greenland, which is
overcompensated for by a strong increase of meltwater production in the lower
areas. We calculate the changes of water fluxes into the adjacent seas
according the simulated surface mass balances changes. The calculated
freshwater flux at the end of the 21st century appears too weak to
induce a significant reduction of the meridional overturning circulation in
the North Atlantic. The resulting surface mass balance decrease between the
last decades of the 20th and 21st centuries is equivalent
to a positive contribution of 0.8 mm yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt; to global eustatic sea-level
rise.</abstract>
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</article>

