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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>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-495-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/495/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/495/2010/tcd-4-495-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/495/2010/tcd-4-495-2010.pdf</fulltext_pdf>
	<start_page>495</start_page>
	<end_page>560</end_page>
	<publication_date>2010-04-08</publication_date>
	<article_title content_type="html">Manufactured analytical solutions for isothermal full-Stokes ice sheet models</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Sargent</name>
			<email>asarge21maine.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. L. Fastook</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Climate Change Institute, University of Maine, Orono, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We present the detailed construction of an exact solution to time-dependent
and steady-state isothermal full-Stokes ice sheet problems. The solutions are
constructed for two-dimensional flowline and three-dimensional full-Stokes
ice sheet models with variable viscosity. The construction is done by
choosing for the specified ice surface and bed a velocity distribution that
satisfies both mass conservation and the kinematic boundary conditions. Then
a compensatory stress term in the conservation of momentum equations and
their boundary conditions is calculated to make the chosen velocity
distributions as well as the chosen pressure field into exact solutions. By
substituting different ice surface and bed geometry formulas into the derived
solution formulas, analytical solutions for different geometries can be
constructed.
&lt;br&gt;&lt;br&gt;
The boundary conditions can be specified as essential Dirichlet conditions or
as periodic boundary conditions. By changing a parameter value, the
analytical solutions allow investigation of algorithms for a different range
of aspect ratios as well as for different, frozen or sliding, basal
conditions. The analytical solutions can also be used to estimate the
numerical error of the method in the case when the effects of the boundary
conditions are eliminated, that is, when the exact solution values are
specified as inflow and outflow boundary conditions.</abstract>
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</article>

