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	<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>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-1497-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1497/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1497/2010/tcd-4-1497-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1497/2010/tcd-4-1497-2010.pdf</fulltext_pdf>
	<start_page>1497</start_page>
	<end_page>1523</end_page>
	<publication_date>2010-08-27</publication_date>
	<article_title content_type="html">Parameterization for subgrid-scale motion of ice-shelf calving-fronts</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>T. Albrecht</name>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>M. Martin</name>
		</author>
		<author numeration="3" affiliations="1,3">
			<name>M. Haseloff</name>
		</author>
		<author numeration="4" affiliations="1,2">
			<name>R. Winkelmann</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>A. Levermann</name>
			<email>anders.levermann@pik-potsdam.de</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Earth System Analysis, Potsdam Institute for Climate Impact Research, Potsdam, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Physics, University of Potsdam, Potsdam, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Earth and Ocean Science, University of British Columbia, Vancouver, Canada</affiliation>
	</affiliations>
	<abstract content_type="html">A parameterization for the motion of ice-shelf fronts on a Cartesian
      grid in finite-difference land-ice models is presented. The scheme
      prevents artificial thinning of the ice shelf at its edge, which
      occurs due to the finite resolution of the model. The intuitive
      numerical implementation diminishes numerical dispersion at the ice
      front and enables the application of physical boundary conditions to
      improve the calculation of stress and velocity fields throughout the
      ice-sheet-shelf system. Numerical properties of this subgrid
      modification are assessed in the Potsdam Parallel Ice Sheet Model
      (PISM-PIK) for different geometries in one and two horizontal
      dimensions and are verified against an analytical solution in a
      flow-line setup.</abstract>
	<references>
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</article>

