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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>3</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/tcd-3-805-2009</doi>
	<article_url>http://www.the-cryosphere-discuss.net/3/805/2009/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/3/805/2009/tcd-3-805-2009.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/3/805/2009/tcd-3-805-2009.pdf</fulltext_pdf>
	<start_page>805</start_page>
	<end_page>829</end_page>
	<publication_date>2009-09-29</publication_date>
	<article_title content_type="html">Interaction between ice sheet dynamics and subglacial lake circulation: a coupled modelling approach</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>M. Thoma</name>
			<email>malte.thoma@awi.de</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>K. Grosfeld</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. Mayer</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>F. Pattyn</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Bavarian Academy and Sciences, Commission for Glaciology, Alfons-Goppel-Str. 11, 80539  Munich, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Alfred Wegener Institute for Polar and Marine Research, Bussestrasse 24, 27570  Bremerhaven, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Laboratoire de Glaciologie, DÃ©partement des Sciences de la Terre et de l&apos;Environnement  (DSTE), UniversitÃ© Libre de Bruxelles (ULB), CP 160/03, Avenue F.D. Roosevelt, 1050 Bruxelles,  Belgium</affiliation>
	</affiliations>
	<abstract content_type="html">Subglacial lakes in Antarctica influence to a large extent the flow of the ice sheet. In
this study we use an idealised lake geometry to study this impact.  We employ a) an improved
three-dimensional full Stokes ice flow model with a nonlinear rheology, b)
a three-dimensional fluid dynamics model with eddy diffusion to simulate basal mass balance,
and c) a newly developed coupler to exchange boundary conditions between individual models.
Different boundary conditions are applied over grounded ice and floating ice. This results in
significantly increased temperatures within the ice on top of the lake, compared to ice at
the same depth outside the lake area. Basal melting of the ice sheet increases this lateral
temperature gradient.  Upstream the ice flow converges towards the lake and accelerates by
about 10% whenever basal melting at the iceâ€“lake boundary is present. Above and downstream
of the lake, where the ice flow diverges, a velocity decrease of about 10% is simulated.</abstract>
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