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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>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-2053-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/2053/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/2053/2009/cpd-5-2053-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/2053/2009/cpd-5-2053-2009.pdf</fulltext_pdf>
	<start_page>2053</start_page>
	<end_page>2080</end_page>
	<publication_date>2009-07-29</publication_date>
	<article_title content_type="html">The importance of paleoclimate modelling for improving predictions of future climate change</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. C. Hargreaves</name>
			<email>jules@jamstec.go.jp</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. D. Annan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Global Change Projection Research Program, Research Institute for Global Change, JAMSTEC,  3173-25 Showa-machi, Kanazawa-ku, Yokohama City, Kanagawa, 236-0001, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">We use an ensemble of runs from the MIROC3.2 AGCM with slab-ocean to explore the extent to
      which mid-Holocene simulations are relevant to predictions of future climate change. The
      results are compared with similar analyses for the Last Glacial Maximum (LGM) and
      pre-industrial control climate. We find evidence that the paleoclimate epochs can provide
      some independent validation of the models that is also relevant for future
      predictions. Considering the paleoclimate epochs, we find that the stronger global forcing
      and hence larger climate change at the LGM makes this likely to be the more powerful one for
      estimating the large-scale changes that are anticipated due to anthropogenic forcing. The
      regions from the mid-Holocene simulations which produce significant results (mid to high
      northern latitude land temperature and monsoon precipitation) do, however, coincide with
      areas where the LGM results are weak, and are also areas where the paleodata indicate
      significant climate changes have occurred. Thus, these areas should be a high priority for
      model improvement and validation.</abstract>
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</article>

