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	<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-5-1751-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/1751/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/1751/2009/cpd-5-1751-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/1751/2009/cpd-5-1751-2009.pdf</fulltext_pdf>
	<start_page>1751</start_page>
	<end_page>1762</end_page>
	<publication_date>2009-07-01</publication_date>
	<article_title content_type="html">Strong indications for nonlinear dynamics during Dansgaard-Oeschger events</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>H. Braun</name>
			<email>holger.braun@iup.uni-heidelberg.de</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Heidelberg Academy of Sciences and Humanities, Heidelberg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Denmark</affiliation>
	</affiliations>
	<abstract content_type="html">Many climate records show the occurrence of large amplitude (10–15 K),
millennial-scale warming events during glacial times, the Dansgaard-Oeschger
(DO) events. So far these events have almost exclusively been investigated
by means of linear time series analysis. The scope of this paper is to test
if the assumption of linearity is fulfilled during DO events. By means of a
surrogate-based Monte Carlo method, I here demonstrate that the 60 000-year
long &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O-record from the NGRIP ice core from Greenland allows
to reject the null hypothesis of linearity beyond any reasonable level of
doubt. Instead, the ice core record supports the interpretation that the
events represent regime switches between different states of operation of
glacial climate. As a conclusion, future studies on DO events should focus
on the development and the application of more adequate (i.e., nonlinear)
methods of time series analysis.</abstract>
	<references>
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</article>

