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	<journal>
		<journal_title>The Cryosphere</journal_title>
		<journal_url>www.the-cryosphere.net</journal_url>
		<issn>1994-0416</issn>
		<eissn>1994-0424</eissn>
		<volume_number>4</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tc-4-147-2010</doi>
	<article_url>http://www.the-cryosphere.net/4/147/2010/</article_url>
	<abstract_html>http://www.the-cryosphere.net/4/147/2010/tc-4-147-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere.net/4/147/2010/tc-4-147-2010.pdf</fulltext_pdf>
	<start_page>147</start_page>
	<end_page>160</end_page>
	<publication_date>2010-04-28</publication_date>
	<article_title content_type="html">Polynyas in a dynamic-thermodynamic sea-ice model</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. Ö. Ólason</name>
			<email>einar.olason@zmaw.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>I. Harms</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Centre for Marine and Atmospheric Research, Institute of Oceanography, University of Hamburg,  Hamburg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The representation of polynyas in viscous-plastic dynamic-thermodynamic sea-ice models is studied
      in a simplified test domain, in order to give recommendations about parametrisation choices.
      Bjornsson et al. (2001) validated their dynamic-thermodynamic model against a polynya
      flux model in a similar setup and we expand on that work here, testing more sea-ice rheologies and
      new-ice thickness formulations. The two additional rheologies tested give nearly identical results
      whereas the two new-ice thickness parametrisations tested give widely different results. Based on
      our results we argue for using the new-ice thickness parametrisation of Hibler (1979). We also
      implement a new parametrisation for the parameter &lt;i&gt;h&lt;/i&gt;&lt;sup&gt;0&lt;/sup&gt; from Hibler&apos;s scheme, based on ideas from a
      collection depth parametrisation for flux polynya models.</abstract>
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</article>

