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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>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-2223-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/2223/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/2223/2009/cpd-5-2223-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/2223/2009/cpd-5-2223-2009.pdf</fulltext_pdf>
	<start_page>2223</start_page>
	<end_page>2237</end_page>
	<publication_date>2009-09-30</publication_date>
	<article_title content_type="html">Potential analysis reveals changing number of climate states during  the last 60 kyr</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. N. Livina</name>
			<email>v.livina@uea.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>F. Kwasniok</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. M. Lenton</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Environmental Sciences, University of  East Anglia, Norwich, UK</affiliation>
		<affiliation numeration="2" content_type="html">School of Engineering, Computing and Mathematics,  University of Exeter, Exeter, UK</affiliation>
	</affiliations>
	<abstract content_type="html">We develop and apply a new statistical method of potential analysis
for detecting the
number of states of a geophysical
system, from its recorded time series. Estimation of the degree of a
polynomial potential allows us to derive the number of potential
wells in a system. The method correctly detects changes in the number of wells
in artificial data. In ice-core proxy records of Greenland
paleotemperature, a reduction in the number of climate states from
two to one is
detected sometime prior to the last glacial maximum (LGM),
23–19 kyr BP.
This  bifurcation can be interpreted as loss of
stability of the warm interstadial state of the Dansgaard-Oeschger
events. In data spanning the last
glacial termination, up to four climate states are detected,
plausibly representing the LGM, Bolling-Allerod,
Younger Dryas, and the Holocene.
The proposed method can be applied to a wide
range of geophysical time series exhibiting bifurcations.</abstract>
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</article>

