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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>3</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-1167-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/1167/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/1167/2007/cpd-3-1167-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/1167/2007/cpd-3-1167-2007.pdf</fulltext_pdf>
	<start_page>1167</start_page>
	<end_page>1198</end_page>
	<publication_date>2007-10-26</publication_date>
	<article_title content_type="html">Reconstructing glacier-based climates of LGM Europe and Russia &amp;ndash; Part 2: A dataset of LGM climates derived from degree-day modelling of palaeo glaciers</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>R. Allen</name>
			<email>robert.allen@landmarkinfo.co.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. J. Siegert</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. J. Payne</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Geographical Sciences, University of Bristol, University Road, Bristol, BS8 1SS, UK</affiliation>
		<affiliation numeration="2" content_type="html">School of GeoSciences, University of Edinburgh, Grant Institute, King&apos;s Buildings, West Mains Road, Edinburgh, EH9 3JW, UK</affiliation>
		<affiliation numeration="3" content_type="html">now at: Landmark Information Group, 5-7 Abbey Court, Eagle Way, Sowton, Exeter, EX2 7HY, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The study of European and Russian Quaternary glacial-geological evidence
during the last 15 years has generated sufficient to data to use former
glacial extent as a proxy for Last Glacial Maximum (LGM) climate at a
continental scale. Utilisation of such data is relevant for two reasons.
First, continental to global scale proxy reconstructions of past climate are
an important tool in the assessment of retrospective general circulation
model (GCM) simulations. Second, the development of a multi-proxy approach
will result in a more robust proxy based climate signal. A new and
independent dataset of 36 LGM climate estimates derived from European and
Russian mountain regions is presented in this paper. A simple
glacier-climate model was used to establish the optimum LGM climate
conditions for each region from a suite of over 4000 model climates using
the principle of zero cumulative mass balance. Clear regional trends are
present in the reconstructed LGM climates; temperature anomalies north of
the Alps are 2&amp;deg;C and 5&amp;deg;C larger than those in the western and
eastern Mediterranean, respectively. In Russia the model results suggest
that both the Arctic Urals and Puterana Plateau were probably glaciated by
small mountain glaciers during the LGM.</abstract>
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</article>

