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<article language="en">
	<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>2</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/cp-2-131-2006</doi>
	<article_url>http://www.clim-past.net/2/131/2006/</article_url>
	<abstract_html>http://www.clim-past.net/2/131/2006/cp-2-131-2006.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/2/131/2006/cp-2-131-2006.pdf</fulltext_pdf>
	<start_page>131</start_page>
	<end_page>136</end_page>
	<publication_date>2006-10-12</publication_date>
	<article_title content_type="html">Equatorial insolation: from precession harmonics to eccentricity frequencies</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Berger</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. F. Loutre</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J. L. Mélice</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Université catholique de Louvain, Institut d&apos;Astronomie et de  Géophysique G. Lemaître, 2 Chemin du Cyclotron, 1348  Louvain-la-Neuve, Belgium</affiliation>
		<affiliation numeration="2" content_type="html">Institut de Recherche pour le Développement, Department of Oceanography, University of Cape Town, Rondebosch 7701,  South Africa</affiliation>
	</affiliations>
	<abstract content_type="html">Since the paper by Hays et al.&amp;nbsp;(1976), spectral analyses of climate proxy
records provide substantial evidence that a fraction of the climatic
variance is driven by insolation changes in the frequency ranges of
obliquity and precession variations. However, it is the variance components
centered near 100&amp;nbsp;kyr which dominate most Upper Pleistocene climatic
records, although the amount of insolation perturbation at the eccentricity
driven periods close to 100-kyr (mainly the 95&amp;nbsp;kyr- and 123&amp;nbsp;kyr-periods)
is much too small to cause directly a climate change of ice-age amplitude.
Many attempts to find an explanation to this 100-kyr
cycle in climatic records have been made over the last decades. Here we show
that the double maximum which characterizes the daily irradiation received
in tropical latitudes over the course of the year is at the origin in
equatorial insolation of not only strong 95&amp;nbsp;kyr and 123&amp;nbsp;kyr periods
related to eccentricity, but also of a 11-kyr and a
5.5-kyr periods related to precession.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Bard, E. and Frank, M.: Climate change and solar variability, What is new under the Sun, Earth Planet. Sci. Lett., 248, 280&amp;ndash;298, 2006. </reference>
		<reference numeration="2" content_type="text"> Berger, A.: Long-term variations of daily insolation and Quaternary climatic changes, J. Atmos. Sci., 35(12), 2362&amp;ndash;2367, 1978. </reference>
		<reference numeration="3" content_type="text"> Berger, A., Loutre, M. F., and Tricot, Ch.: Insolation and Earth&apos;s orbital periods, J. Geophys. Res., 98(D6), 10 341&amp;ndash;10 362, 1993. </reference>
		<reference numeration="4" content_type="text"> Berger, A. and Loutre, M. F.: Intertropical latitudes and precessional and half-precessional cycles, Science, 278(5342), 1476&amp;ndash;1478, 1997. </reference>
		<reference numeration="5" content_type="text"> Berger, A., Loutre, M. F., and Mélice, J. L.: Instability of the astronomical periods from 1.5 Myr BP to 0.5 Myr AP, Palaeoclimates, Data and Modelling, 2(4), 239&amp;ndash;280, 1998. </reference>
		<reference numeration="6" content_type="text"> Bush, M. B., Moreno, E., de Oliveira, P. E., and Colinvaux, P. A.: Orbital-forcing signal in sediments of two Amazonian lakes, J. Paleolim., 27, 341&amp;ndash;352, 2002. </reference>
		<reference numeration="7" content_type="text"> Claussen, M., Fohlmeister, J., Ganopolsky, A., and Brovkin, V.: Vegetation dynamics amplifies precessional forcing, Geophysical Research Letters, 33(9), L09709; doi:10.1029/2006GL0266111, 2006. </reference>
		<reference numeration="8" content_type="text"> Clemens, S., Prell, W., Murray, D., Shimmield, G., and Weedon, G.: Forcing mechanisms of the Indian Ocean monsoon, Nature, 353, 720&amp;ndash;725, 1991. </reference>
		<reference numeration="9" content_type="text"> Clemens, S.: Dust response to seasonal atmospheric forcing: Proxy evaluation and calibration, Paleoceanography, 13, 471&amp;ndash;490, 1998. </reference>
		<reference numeration="10" content_type="text"> Clement, A. C., Hall, A., and Broccoli, A. J.: The importance of precessional signals in the tropical climate, Clim. Dyn., 22, 327&amp;ndash;341, 2004. </reference>
		<reference numeration="11" content_type="text"> Cruz Jr., F. W., Burns, S. J., Karmann, I., Sharp, W. D., Vuille, M., Cardoso, A. O., Ferrari, J. A., Silva Dias, P. L., and Viana, O.: Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil, Nature, 434, 63&amp;ndash;66, 2005. </reference>
		<reference numeration="12" content_type="text"> de Garidel-Thoron, Th., Rosenthal, Y., Bassinot, F., and Beaufort, L.: Stable sea surface temperatures in the Western Pacific warm pool over the past 1.75 million years, Nature, 433(7023), 294&amp;ndash;298, 2005. </reference>
		<reference numeration="13" content_type="text"> deMenocal, P.: Plio-Pleistocene African Climate, Science, 270, 53&amp;ndash;59, 1995. </reference>
		<reference numeration="14" content_type="text"> deMenocal, P.: African climate change and faunal evolution during the Pliocene-Pleistocene, Earth Planet. Sci. Lett., 220, 3&amp;ndash;24, 2004. </reference>
		<reference numeration="15" content_type="text"> Fröhlich, C. and Lean, J.: Solar radiative output and its variability: evidence and mechanisms, Astron. Astrophys. Rev., 12, 273&amp;ndash;320, 2004. </reference>
		<reference numeration="16" content_type="text"> Hagelberg, T. K., Bond, G., and de Menocal, P.: Milankovitch band forcing of sub-Milankovitch climate variability during the Pleistocene, Paleoceanography, 9(4), 545&amp;ndash;558, 1994. </reference>
		<reference numeration="17" content_type="text"> Hays, J. D., Imbrie, J., and Shackleton, N. J.: Variations in the Earth&apos;s orbit: pacemaker of the Ice Ages, Science, 194, 1121&amp;ndash;1132, 1976. </reference>
		<reference numeration="18" content_type="text"> Kerr, R. A.: The Tropics return to the climate system, Sciences, 292(5517), 660&amp;ndash;661, 2001. </reference>
		<reference numeration="19" content_type="text"> Kerr, R. A.: Tropical Pacific a key to deglaciation, Science, 299(5604), 183&amp;ndash;184, 2003. </reference>
		<reference numeration="20" content_type="text"> Leuschner, D. C. and Sirocko, F.: Orbital insolation forcing of the Indian Monsoon &amp;ndash; a motor for global climate changes?, Palaeogeography, Palaeoclimatology, Palaeoecology, 197(1&amp;ndash;2), 83&amp;ndash;95, 2003. </reference>
		<reference numeration="21" content_type="text"> Lorenz, S. J., Kim, J. H., Rimbu, N., Schneider, R. R., and Lohmann, G.: Orbitally driven insolation forcing on Holocene climate trends: evidence from alkenone data and climate modelling, Paleoceanography, 21, PA1002, doi:10.1029/2005PA001152, 2006. </reference>
		<reference numeration="22" content_type="text"> Maslin, M. A. and Burns, S. J.: Reconstruction of the Amazon Basin effective moisture availability over the last 14,000 years, Science, 290, 2285&amp;ndash;2287, 2000.  </reference>
		<reference numeration="23" content_type="text"> McIntyre, A. and Molfino, B.: Forcing of Atlantic equatorial and subpolar millennial cycles by precession, Science, 274(5294), 1867&amp;ndash;1870, 1996. </reference>
		<reference numeration="24" content_type="text"> Milankovitch, M.: Kanon der Erdbestrahlung und seine Anwendung auf das Eiszeitenproblem, Royal Serbian Sciences, Spec. pub. 132, section of Mathematical and Natural Sciences, vol. 33, pp. 633, Belgrade, 1941; (&quot;Canon of Insolation and the Ice Age problem&quot;, English Translation by Isra\&quot;el Program for Scientific Translation and published for the U.S.&amp;nbsp;Department of Commerce and the National Science Foundation, Washington D.C., 1969, and by Zavod za Ud\vzbenike i Nastavna Sredstva in cooperation with Muzej nauke i tehnike Srpske akademije nauka i umetnosti, Beograd, 1998). </reference>
		<reference numeration="25" content_type="text"> Murphy, J. J.: The glacial climate and the polar ice-cap, Quarterly Journal Geological Society, 32, 400&amp;ndash;406, 1876. </reference>
		<reference numeration="26" content_type="text"> PMIP2: http://www-lsce.cea.fr/pmip2/. </reference>
		<reference numeration="27" content_type="text"> Peeters, F. J. C., Acheson, R., Brummer, G. J. A., de Ruijter, W. P. M., Schneider, R. R., Ganssen, G. M., Ufkes, E., and Kroon, D.: Vigorous exchange between the Indian and Atlantic ocean at the end of the past five glacial periods, Nature, 430(7000), 661&amp;ndash;665, 2004. </reference>
		<reference numeration="28" content_type="text"> Reuning, L., Reijmer, J. J. G., Betzler, Ch., Timmermann, A., and Steph, S.: Sub-Milankovitch cycles in periplatform carbonates from the early Pliocene Great Bahama Bank, Paleoceanography, 21, PA1017, doi:10.1029/2004PA001075, 2006. </reference>
		<reference numeration="29" content_type="text"> Rossignol-Strick, M., Paterne, M., Bassinot, F. C., Emeis, K.-C., and de Lange, G. J.: An unusual mid-Pleistocene monsoon period over Africa and Asia, Nature, 392, 269&amp;ndash;272, 1998. </reference>
		<reference numeration="30" content_type="text"> Ruddiman, W. F.: What ist he timing of orbital-scale monsoon changes?, Quaternary Science Review, 25(7&amp;ndash;8), 657&amp;ndash;658, 2006. </reference>
		<reference numeration="31" content_type="text"> Solanki, S. K., Usoskin, I. G., Kromer, B., Schüssler, M., and Beer, J.: Unusual activity of the Sun during recent decades compared to the previous 11,000 year, Nature, 431, 1084&amp;ndash;1087, doi:10.1038/nature02995, 2004. </reference>
		<reference numeration="32" content_type="text"> Sun, J. and Huang, X.: Half-precession cycles recorded in Chinese loess: response to low-latitude insolation forcing during the Last Interglaciation, Quaternary Science Reviews, 25(9&amp;ndash;10), 1065&amp;ndash;1972, 2006. </reference>
		<reference numeration="33" content_type="text"> Trauth, M. H., Deino, A., Bergner, A. G. N., and Strecker, M. R.: East African climate change and orbital forcing during the last 175 kyr BP, Earth Planet. Sci. Lett., 206, 297&amp;ndash;313, 2003. </reference>
		<reference numeration="34" content_type="text"> Tuenter, E., Weber, S. L., Hilgen, F. J., and Lourens, L. J.: Simulating sub-Milankovitch climate variations associated with vegetation dynamics, Clim. Past Discuss., 2, 745&amp;ndash;769, 2006. </reference>
		<reference numeration="35" content_type="text"> Turney, C. S. M., Kershaw, A. P., Clemens, S. C., Branch, N., Moss, P. T., and Fifield, L. K.: Millennial and orbital variations of El Ni&amp;nbsp;no/Southern oscillation and high-latitude climate in the last glacial period, Nature, 428(6980), 306&amp;ndash;310, 2004. </reference>
	</references>
</article>

