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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>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/tcd-2-601-2008</doi>
	<article_url>http://www.the-cryosphere-discuss.net/2/601/2008/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/2/601/2008/tcd-2-601-2008.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/2/601/2008/tcd-2-601-2008.pdf</fulltext_pdf>
	<start_page>601</start_page>
	<end_page>622</end_page>
	<publication_date>2008-07-16</publication_date>
	<article_title content_type="html">The emergence of surface-based Arctic amplification</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. C. Serreze</name>
			<email>serreze@nsidc.org</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. P. Barrett</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. C. Stroeve</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>D. N. Kindig</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. M. Holland</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Snow and Ice Data Center, Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">Climate and Global Dynamics Division, Earth and Sun Systems Laboratory, National Center for Atmospheric Research, Boulder CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Rises in surface and lower troposphere air temperatures through the 21st
century are projected to be especially pronounced over the Arctic Ocean
during the cold season. This Arctic amplification is largely driven by loss
of the sea ice cover, allowing for strong heat transfers from the ocean to
the atmosphere. Consistent with observed reductions in sea ice extent,
fields from the NCEP/NCAR reanalysis suggest emergence of surface-based
Arctic amplification in the last decade.</abstract>
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</article>

