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	<journal>
		<journal_title>Ocean Science</journal_title>
		<journal_url>www.ocean-sci.net</journal_url>
		<issn>1812-0784</issn>
		<eissn>1812-0792</eissn>
		<volume_number>2</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/os-2-201-2006</doi>
	<article_url>http://www.ocean-sci.net/2/201/2006/</article_url>
	<abstract_html>http://www.ocean-sci.net/2/201/2006/os-2-201-2006.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/2/201/2006/os-2-201-2006.pdf</fulltext_pdf>
	<start_page>201</start_page>
	<end_page>211</end_page>
	<publication_date>2006-10-23</publication_date>
	<article_title content_type="html">Results from the implementation of the Elastic Viscous Plastic sea ice rheology in HadCM3</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>W. M. Connolley</name>
			<email>wmc@bas.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. B. Keen</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. J. McLaren</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK</affiliation>
		<affiliation numeration="2" content_type="html">Met Office Hadley Centre, FitzRoy Road, Exeter, EX1 3PB, UK</affiliation>
	</affiliations>
	<abstract content_type="html">We present results of an implementation of the Elastic Viscous Plastic (EVP)
sea ice dynamics scheme into the Hadley Centre coupled ocean-atmosphere
climate model HadCM3. Although the large-scale simulation of sea ice in
HadCM3 is quite good with this model, the lack of a full dynamical model
leads to errors in the detailed representation of sea ice and limits our
confidence in its future predictions. We find that introducing the EVP
scheme results in a worse initial simulation of the sea ice. This paper
documents various enhancements made to improve the simulation, resulting in
a sea ice simulation that is better than the original HadCM3 scheme overall.
Importantly, it is more physically based and provides a more solid
foundation for future development. We then consider the interannual
variability of the sea ice in the new model and demonstrate improvements
over the HadCM3 simulation.</abstract>
	<references>
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</article>

