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	<journal>
		<journal_title>Climate of the Past</journal_title>
		<journal_url>www.clim-past.net</journal_url>
		<issn>1814-9324</issn>
		<eissn>1814-9332</eissn>
		<volume_number>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cp-3-129-2007</doi>
	<article_url>http://www.clim-past.net/3/129/2007/</article_url>
	<abstract_html>http://www.clim-past.net/3/129/2007/cp-3-129-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/3/129/2007/cp-3-129-2007.pdf</fulltext_pdf>
	<start_page>129</start_page>
	<end_page>134</end_page>
	<publication_date>2007-02-28</publication_date>
	<article_title content_type="html">The DO-climate events are probably noise induced: statistical investigation of the claimed 1470 years cycle</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. D. Ditlevsen</name>
			<email>pditlev@gfy.ku.dk</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>K. K. Andersen</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. Svensson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">The Niels Bohr Institute, Department of Geophysics, University of Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen O, Denmark</affiliation>
	</affiliations>
	<abstract content_type="html">The significance of the apparent 1470 years cycle in the recurrence of
the Dansgaard-Oeschger (DO) events, observed in the Greenland ice cores,
is debated. Here we present statistical significance
tests of this periodicity.
The detection of a periodicity relies strongly on the accuracy of the
dating of the DO events. Here we use both the new NGRIP GICC05 time scale based
on multi-parameter annual layer counting and the GISP2 time scale where
the periodicity is most pronounced. For the NGRIP dating the recurrence
times are indistinguishable from a random occurrence. This is also the
case for the GISP2 dating, except in the case where the DO9 event is
omitted from the record.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Alley, R B., Shuman, C A., Meese, D A., Gow, A J., Taylor, K C., Cuffey, K M., Fitzpatrick, J J., Grootes, P M., Zielinski, G A., Ram, M., Spinelli, G., and Elder, B.: Visual-stratigraphic dating of the GISP2 ice core: Basis, reproducibility and application, J. Geophys. Res., 102, 26 367&amp;ndash;26 381, 1997. </reference>
		<reference numeration="2" content_type="text"> Alley, R B., Anandakrishnan, S., and Jung, P.: Stochastic resonance in the North Atlantic, Paleoceanography, 16, 190&amp;ndash;198, 2001. </reference>
		<reference numeration="3" content_type="text"> Andersen, K K., Svensson, A., Rasmussen, S O., Steffensen, J P., Johnsen, S., Bigler, M., Röthlisberger, R., Ruth, U., Siggaard-Andersen, M.-L., Dahl-Jensen, D., Vinter, B M., and Clausen, H B.: The Greenland Ice Core Chronology 2005, 15&amp;ndash;42 ka. Part 1: Construction of the time scale, QSR Shackleton special edition, 25, 3246&amp;ndash;3257, 2006. </reference>
		<reference numeration="4" content_type="text"> Benzi, R., Parisi, G., Sutera, A., and Vulpiani, A.: Stochasic resonance in climate change, Tellus, 34, 10&amp;ndash;16, 1982. </reference>
		<reference numeration="5" content_type="text"> Braun, H., Christi, M., Rahmstorf, S., Ganopolski, A., Mangini, A., Kubatski, C., Roth, K., and Kromer, B.: Possible solar origin of the 1,470-year glacial climate cycle demonstrated in a coupled model, Nature, 438, 208&amp;ndash;211, 2005. </reference>
		<reference numeration="6" content_type="text"> Dansgaard, W., Johnsen, S J., Clausen, H B., Dahl-Jensen, D., Gundestrup, N S., Hammer, C U., Hvidberg, C S., Steffensen, J P., Sveinbjornsdottir, A E., Jouzel, J., and Bond, G.: Evidence for general instability of past climate from a 250-kyr ice-core record, Nature, 364, 218&amp;ndash;220, 1993. </reference>
		<reference numeration="7" content_type="text"> Ditlevsen, P D., Kristensen, M S., and Andersen, K K.: The recurrence time of Dansgaard-Oeschger events and limits on the possible periodic component, J. Climate, 18, 2594&amp;ndash;2603, 2005. </reference>
		<reference numeration="8" content_type="text"> Grootes, P M. and Stuiver, M.: Oxygen 18/16 variability in Greenland snow and ice with $10^-3$- to $10^5$-year time resolution, J. Geophys. Res., 102, 26 455&amp;ndash;26 470, 1997. </reference>
		<reference numeration="9" content_type="text"> Huybers, P. and Wunsch, C.: Obliquity pacing of the late Pleistocene glacial terminations, Nature, 434, 491&amp;ndash;494, 2005. </reference>
		<reference numeration="10" content_type="text"> Johnsen, S J., Dahl-Jensen, D., Gundestrup, N., Steffensen, J P., Clausen, H B., Miller, H., Masson-Delmotte, V., Sveinbjørnsdottir, A E., and White, J.: Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP, J. Quat. Sci., 16, 299&amp;ndash;307, 2001. </reference>
		<reference numeration="11" content_type="text"> Meese, D A., Gow, A J., Alley, R B., Zielinski, G A., Grootes, P M., Ram, M., Taylor, K C., Mayewski, P A., and Bolzan, J F.: The Greenland Ice Sheet Project 2 depth-age scale: Methods and results, J. Geophys. Res., 102, 26 411&amp;ndash;26 423, 1997. </reference>
		<reference numeration="12" content_type="text"> Muscheler, R. and Beer, J.: Solar forced Dansgaard/Oeschger events?, Geophys. Res. Lett., 33, L20706, doi:10.1029/2006GL026779, 2006. </reference>
		<reference numeration="13" content_type="text"> North GRIP members: High resolution Climate Record of the Northern Hemisphere reaching into the last Glacial Interglacial Period, Nature, 431, 147&amp;ndash;151, 2004. </reference>
		<reference numeration="14" content_type="text"> Rahmstorf, S.: Timing of abrupt climate changes: A precise clock, Geophys. Res. Lett., 30, 1510&amp;ndash;1514, 2003. </reference>
		<reference numeration="15" content_type="text"> Schulz, M.: On the 1470-year pacing of Dansgaard-Oeschger warm events, Paleoceanography, 17, doi:1029/200PA000571, 2002. </reference>
		<reference numeration="16" content_type="text"> Svensson, A., Andersen, K K., Bigler, M., Clausen, H B., Dahl-Jensen, D., Johnsen, S., Muscheler, R., Rasmussen, S O., Röthlisberger, R., Steffensen, J P., and Vinter, B M.: The Greenland Ice Core Chronology 2005, 15&amp;ndash;42 ka. Part 2: Comparison to other records, QSR Shackleton special edition, 25, 3258&amp;ndash;3267, 2006. </reference>
		<reference numeration="17" content_type="text"> Wunsch, C.: On sharp spectral lines in the climate record and the millennial peak, Paleoceanography, 15, 417&amp;ndash;424, 2000. </reference>
	</references>
</article>

