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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>4</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-321-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/321/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/321/2010/tcd-4-321-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/321/2010/tcd-4-321-2010.pdf</fulltext_pdf>
	<start_page>321</start_page>
	<end_page>345</end_page>
	<publication_date>2010-03-24</publication_date>
	<article_title content_type="html">Increasing runoff from the Greenland Ice Sheet at Kangerlussuaq (Søndre Strømfjord) in a 30-year perspective, 1979&amp;ndash;2008</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. H. Mernild</name>
			<email>mernild@lanl.gov</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>G. E. Liston</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>K. Steffen</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>M. van den Broeke</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>B. Hasholt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Climate, Ocean, and Sea Ice Modeling Group, Computational Physics and Methods (CCS-2), Los Alamos National Laboratory, New Mexico, USA</affiliation>
		<affiliation numeration="2" content_type="html">Cooperative Institute for Research in the Atmosphere,Colorado State University, Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">Cooperative Institute for Research in Environmental Sciences, University of Colorado, Colorado, USA</affiliation>
		<affiliation numeration="4" content_type="html">Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, Holland</affiliation>
		<affiliation numeration="5" content_type="html">Department of Geography and Geology, University of Copenhagen, Copenhagen, Denmark</affiliation>
	</affiliations>
	<abstract content_type="html">This observation and modeling study provides insights into runoff exiting the
Watson River drainage basin, Kangerlussuaq, West Greenland during a 30 year
period (1978/79–2007/08) when the climate experienced increasing
temperatures and precipitation. The 30-year simulations quantify the
terrestrial freshwater output from part of the Greenland Ice Sheet (GrIS) and
the land between the GrIS and the ocean, in the context of global warming and
increasing GrIS surface melt. We used a snow-evolution modeling system
(SnowModel) to simulate the winter accumulation and summer ablation
processes, including runoff and surface mass balance (SMB), of the ice sheet.
To a large extent, the SMB fluctuations could be explained by changes in net
precipitation (precipitation minus evaporation and sublimation), with 8 out
of 30 years having negative SMB, mainly because of relatively low annual net
precipitation. The overall trend in net precipitation and runoff increased
significantly, while SMB increased insignificantly throughout the simulation
period, leading to enhanced precipitation of 0.59 km&lt;sup&gt;3&lt;/sup&gt; w.eq. (or
60%), runoff of 0.43 km&lt;sup&gt;3&lt;/sup&gt; w.eq. (or 54%), and SMB of
0.16 km&lt;sup&gt;3&lt;/sup&gt; w.eq. (or 86%). Runoff rose on average from
0.80 km&lt;sup&gt;3&lt;/sup&gt; w.eq. in 1978/79 to 1.23 km&lt;sup&gt;3&lt;/sup&gt; w.eq. in 2007/08. The
percentage of catchment outlet runoff explained by runoff from the GrIS
decreased on average &amp;sim;10%.</abstract>
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</article>

