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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>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/tcd-1-123-2007</doi>
	<article_url>http://www.the-cryosphere-discuss.net/1/123/2007/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/1/123/2007/tcd-1-123-2007.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/1/123/2007/tcd-1-123-2007.pdf</fulltext_pdf>
	<start_page>123</start_page>
	<end_page>168</end_page>
	<publication_date>2007-07-03</publication_date>
	<article_title content_type="html">Reconstruction of the 1979&amp;ndash;2006 Greenland ice sheet surface mass balance using the regional climate model MAR</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>X. Fettweis</name>
			<email>fettweis@astr.ucl.ac.be</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut d&apos;Astronomie et de GÃ©ophysique Georges Lema&amp;#x00EE;tre, UniversitÃ© catholique de Louvain, Louvain-la-Neuve, Belgium</affiliation>
	</affiliations>
	<abstract content_type="html">Results from a 28-year simulation (1979&amp;ndash;2006) over the Greenland ice sheet
(GIS) reveal an increase of the solid precipitation (+0.4&amp;plusmn;2.5 km&lt;sup&gt;3&lt;/sup&gt; yr&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) and the run-off (+7.9&amp;plusmn;3.3 km&lt;sup&gt;3&lt;/sup&gt; yr&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) of surface
melt water. The net effect of these competing factors leads to a significant
Surface Mass Balance (SMB) loss rate of &amp;minus;7.2&amp;plusmn;5.1 km&lt;sup&gt;3&lt;/sup&gt; yr&lt;sup&gt;&amp;minus;2&lt;/sup&gt;.
The contribution of changes in the net water vapour fluxes (+0.02&amp;plusmn;0.09 km&lt;sup&gt;3&lt;/sup&gt; yr&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) and rainfall (+0.2&amp;plusmn;0.2 km&lt;sup&gt;3&lt;/sup&gt; yr&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) to
the SMB variability is negligible. The melt water supply has increased
because the GIS surface has been warming up +2.4&amp;deg;C since 1979. Latent
heat flux, sensible heat flux and net solar radiation have not varied
significantly over the last three decades. However, the simulated downward
infra-red flux has increased by 9.3 W m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; since 1979. The natural
climate variability (e.g. the North Atlantic Oscillation) does not explain
these changes on the GIS. The recent global warming, due to the greenhouse
gas concentration increase induced by the human activities, could be a cause
of these changes. The doubling of the surface melt water flux into the ocean
over the period 1979&amp;ndash;2006 suggests that the overall ice sheet mass balance
has been increasingly negative, given the probable meltwater-induced outlet
glacier acceleration. This study suggests that an increased melting dominates
over an increased accumulation in a warming scenario and that the GIS would
likely continue to loose mass in the future. A GIS melting would have an
effect on the stability of the thermohaline circulation (THC) and the global
sea level rise.</abstract>
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