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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>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/tcd-3-77-2009</doi>
	<article_url>http://www.the-cryosphere-discuss.net/3/77/2009/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/3/77/2009/tcd-3-77-2009.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/3/77/2009/tcd-3-77-2009.pdf</fulltext_pdf>
	<start_page>77</start_page>
	<end_page>115</end_page>
	<publication_date>2009-01-22</publication_date>
	<article_title content_type="html">The Gregoriev Ice Cap evolution according to the 2-D ice flowline model for  various climatic scenarios in the future</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. V. Konovalov</name>
			<email>yu-v-k@yandex.ru</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>O. V. Nagornov</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Moscow Engineering Physics Institute (State University), Kashirskoe shosse,  31, 115409 Moscow, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">Different flowline thickness distributions and flowline length
  changes of the Gregoriev Ice Cap were obtained for some surface mass
  balance histories which can be considered as possible surface mass
  balances in the future. The ice cap modeling was performed by
  solving full Stokes equations in the form of one mechanical
  equilibrium equation in terms of stress deviator components in
  couple with continuity equation for incompressible substance.  The
  numerical solution was obtained by the finite-difference method. The
  problem of diagnostic equations stability was overcome by a~compound
  approximation of the ice surface boundary condition based on the
  extending of the mechanical equilibrium equation to ice surface
  points. The problem of stability in the prognostic equation can
  arise at relatively small grid size in horizontal direction in the
  case of steep velocity decreasing closely to the ice front and was
  overcome by introducing the artificial viscosity into the prognostic
  equation. The basal sliding can arise in the glacier tongue at
  certain climatic conditions and was introduced through the linear
  friction law. The correlations between glacier length changes and
  annual air temperature histories were investigated within the
  simplified equation in the form of linear dependence of annual air
  temperature versus the glacier length and time derivation of the
  length.</abstract>
	<references>
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</article>

