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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-3-1199-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/1199/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/1199/2007/cpd-3-1199-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/1199/2007/cpd-3-1199-2007.pdf</fulltext_pdf>
	<start_page>1199</start_page>
	<end_page>1233</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 3: Comparison with GCM and pollen-based climate reconstructions</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">Understanding past climates using GCM models is critical to confidently
predicting future climate change. Although previous analysis of GCM
simulations have shown them to under predicted European glacial temperature
anomalies (the difference between modern and glacial temperatures) such
analyses have focused primarily on results from glacial simulations alone.
Here we compare glacial maximum GCM results with the palaeoenvironment
derived from glacier-climate modelling. The comparison confirms that GCM
anomalies are under predicted, and that this is due to modern conditions
that are modelled too cold and glacial temperatures that are too warm. The
result is that CGM results, if applied to a glacier mass balance model, over
predict the extent of glaciers today, and under predict their extent at the
last glacial (as depicted in glacial geological reconstructions). Effects
such as seasonality and model parameterisation change the magnitude of the
under prediction but still fail to match expected glacial conditions.</abstract>
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</article>

