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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>2</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/tcd-2-759-2008</doi>
	<article_url>http://www.the-cryosphere-discuss.net/2/759/2008/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/2/759/2008/tcd-2-759-2008.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/2/759/2008/tcd-2-759-2008.pdf</fulltext_pdf>
	<start_page>759</start_page>
	<end_page>776</end_page>
	<publication_date>2008-10-28</publication_date>
	<article_title content_type="html">Model resolution influence on simulated sea ice decline</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. O. Sewall</name>
			<email>jos@vt.edu</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geosciences, Virginia Tech, Blacksburg, VA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Satellite observations and model predictions of recent and future Arctic sea
ice decline have raised concerns over the timing and potential impacts of a
seasonally ice-free Arctic Ocean. Model predictions of seasonally ice-free
Arctic conditions are, however, highly variable. Here I present results from
fourteen climate system models from the World Climate Research Programme&apos;s
(WCRP&apos;s) Coupled Model Intercomparison Project phase 3 (CMIP3) multi-model
dataset that indicate modeled Arctic sea ice sensitivity to increased
atmospheric CO&lt;sub&gt;2&lt;/sub&gt; forcing is strongly correlated with ice/ocean model
horizontal resolution. Based on coupled model analyses and ice only
simulations with the Los Alamos National Lab sea ice model (CICE), the
correlation between declining Arctic sea ice cover and ice/ocean model
resolution appears to depend largely on ocean model resolution and its
influence on ocean heat transport into the Arctic basin. The correlation
between model resolution, northward ocean heat transport, and the degree of
Arctic ice loss is independent of ice model physics and complexity. This not
only illustrates one difficulty in using numerical models to accurately
predict the timing and magnitude of Arctic sea ice decline under increasing
atmospheric greenhouse gas forcing, but also highlights one area where
improved simulation (of northward ocean heat transport) could greatly
decrease the uncertainties associated with predictions of future Arctic sea
ice cover.</abstract>
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</article>

