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<article language="en">
	<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>2</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/cpd-2-285-2006</doi>
	<article_url>http://www.clim-past-discuss.net/2/285/2006/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/2/285/2006/cpd-2-285-2006.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/2/285/2006/cpd-2-285-2006.pdf</fulltext_pdf>
	<start_page>285</start_page>
	<end_page>314</end_page>
	<publication_date>2006-06-21</publication_date>
	<article_title content_type="html">The origin of the European &quot;Medieval Warm Period&quot;</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Goosse</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>O. Arzel</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J. Luterbacher</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>M. E. Mann</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>H. Renssen</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>N. Riedwyl</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>A. Timmermann</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>E. Xoplaki</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>H. Wanner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut d’Astronomie et de Géophysique G. Lemaître, Université catholique de Louvain, 2 Chemin du Cyclotron, 1348 Louvain-la-Neuve, Belgium</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Geography and NCCR Climate, University of Bern, Hallerstrasse 12, 3012 Bern, Switzerland</affiliation>
		<affiliation numeration="3" content_type="html">Department of Meteorology and Earth and Environmental Systems Institute (EESI), Pennsylvania State University, University Park, PA16 802-5013, USA</affiliation>
		<affiliation numeration="4" content_type="html">Faculty of Earth and Life Sciences, Vrije Universiteit Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation>
		<affiliation numeration="5" content_type="html">IPRC, SOEST, University of Hawaii, 2525 Correa Road, Honolulu, HI 96 822, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Using a combination of proxy records and results of a three
dimensional climate model, we show that European summer temperatures roughly
a millennium ago were comparable to those of the late 20th century. Those
two relatively mild periods are separated by a rather cold era, supporting
the existence of a summer ``Medieval Warm Period&quot; in Europe. The long-term
temperature history appears to result from the superposition of various
anthropogenic forcings, the summer cooling associated with changes in
land-use over the last 1000 years having the same magnitude as the net
warming due to the combined increase in greenhouse gas concentration and in
sulphate aerosols during the last 200 years. Volcanic and solar forcing
plays a weaker role in this comparison between the late 20th century and the
early second millennium. Evidence for winter is more equivocal. The forced
response in the model displays a clear temperature maximum at the end of the
20th century but the uncertainties are too large to state that this period
is the warmest of the past millennium in Europe in winter.</abstract>
	<references>
	</references>
</article>

