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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>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-99-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/99/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/99/2009/cpd-5-99-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/99/2009/cpd-5-99-2009.pdf</fulltext_pdf>
	<start_page>99</start_page>
	<end_page>125</end_page>
	<publication_date>2009-01-08</publication_date>
	<article_title content_type="html">A few prospective ideas on climate reconstruction: from a statistical single proxy approach towards a multi-proxy and dynamical approach</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>J. Guiot</name>
			<email>guiot@cerege.fr</email>
		</author>
		<author numeration="2" affiliations="3">
			<name>H. B. Wu</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>V. Garreta</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>C. Hatté</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>M. Magny</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CEREGE, CNRS/Aix-Marseille Université UMR6635, BP 80, 13 545 Aix-en-Provence cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">ECCOREV, CNRS/Aix-Marseille Université FR3098, BP 80, 13 545 Aix-en-Provence cedex, France</affiliation>
		<affiliation numeration="3" content_type="html">Institut des Sciences de l&apos;Environnement, UQAM, Montréal PQ, H3C 3P8, Canada</affiliation>
		<affiliation numeration="4" content_type="html">LSCE, CNRS/CEA UMR1572, Domaine du CNRS, 91 198 Gif-sur-Yvette, France</affiliation>
		<affiliation numeration="5" content_type="html">CNRS, UMR6249, Laboratoire Chrono-Environnemment, UFR des Sciences et Techniques, 16 Route de Gray, 25 030 Besanon, France</affiliation>
	</affiliations>
	<abstract content_type="html">Important progresses in palaeoclimatological studies have been made using
statistical methods. But they are in somewhere limited as they take the
present as an absolute reference. The availability of mechanistic models to
simulate the proxies measured in the sediment cores gives now the possibility
to relax this constraint. In particular, vegetation models provide outputs
comparable to pollen data. We present the evolution of the mechanistic
approach based on model inversion with several examples where models are
progressively more sophisticated (from an equilibrium BIOME3 model to
a dynamic LPJ-GUESS model). We show also how it is possible to take into
account several proxies measured on the same core (lake-level status and
&amp;delta;&lt;sup&gt;13&lt;/sup&gt;C) when they are related to a component of the
vegetation. Examples presented concern Last Glacial Maximum in Europe and
Africa, Holocene in a site of the Swiss Jura, an Eemian site in France. The
main results are that: (1) pollen alone is not able to provide exhaustive
information on precipitation, (2) assuming past CO&lt;sub&gt;2&lt;/sub&gt; equivalent to
modern one may induce biases in climate reconstruction, (3) vegetation models
seem to be too much constrained by temperature relative to precipitation in
temperate regions.</abstract>
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