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	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>5</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-1-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/1/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/1/2009/cpd-5-1-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/1/2009/cpd-5-1-2009.pdf</fulltext_pdf>
	<start_page>1</start_page>
	<end_page>27</end_page>
	<publication_date>2009-01-07</publication_date>
	<article_title content_type="html">Potential causes of 15th century Arctic warming using coupled model simulations with data assimilation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. Crespin</name>
			<email>elisabeth.crespin@uclouvain.be</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. Goosse</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. Fichefet</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>M. E. Mann</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Université catholique de Louvain, Institut d&apos;Astronomie et de Géophysique Georges Lemaître, Chemin du Cyclotron, 2, 1348 Louvain la Neuve, Belgium</affiliation>
		<affiliation numeration="2" content_type="html">Department of Meteorology, Department of Geosciences, and Earth and  Environmental Systems Institute, Pennsylvania State University, University  Park, USA</affiliation>
	</affiliations>
	<abstract content_type="html">An ensemble of simulations of the climate of the past millennium
  using a three-dimensional climate model of intermediate complexity
  are constrained to follow temperature histories obtained from
  a recent compilation of well-calibrated surface temperature proxies
  using a simple data assimilation technique. Those simulations
  provide a reconstruction of the climate of the Arctic that is
  compatible with model physics, the forcing applied and the proxy
  records. Available observational data, proxy-based reconstructions
  and our model results suggest that the Arctic climate is
  characterized by substantial variations in surface temperature over
  the past millennium.  Though the most recent decades are likely to
  be the warmest of the past millennium, we find evidence for
  substantial past warming episodes in the Arctic. In particular, our
  model reconstructions show a particularly warm period at the end of
  the 15th century. This warm event is likely related to the
  internal variability of the climate system. We examine the roles of
  competing mechanisms that could potentially produce this anomaly.
  These examinations lead us to conclude that changes in atmospheric
  circulation, through enhanced southwesterly winds towards northern
  Europe, Siberia and Canada, are likely the main cause of the Arctic
  warming during the late 15th century.</abstract>
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