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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>4</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cpd-4-459-2008</doi>
	<article_url>http://www.clim-past-discuss.net/4/459/2008/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/4/459/2008/cpd-4-459-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/4/459/2008/cpd-4-459-2008.pdf</fulltext_pdf>
	<start_page>459</start_page>
	<end_page>493</end_page>
	<publication_date>2008-04-21</publication_date>
	<article_title content_type="html">Monsoon response to changes in Earth&apos;s orbital parameters: comparisons between simulations of the Eemian and of the Holocene</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Braconnot</name>
			<email>pascale.braconnot@cea.fr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>C. Marzin</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>L. Grégoire</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>E. Mosquet</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>O. Marti</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environnement, Unité mixte CEA-CNRS-UVSQ, Orme des Merisiers, bât. 712, 91191 Gif-sur-Yvette Cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">School of Geographical Sciences, Univ. of Bristol, University Road &amp;ndash; Bristol BS8 1SS, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Monsoon is the major manifestation of the seasonal cycle in the tropical
regions, and there is a wide range of evidence from marine and terrestrial
data that monsoon characteristics are affected by changes in the Earth&apos;s
orbital parameters. We consider 3 periods in the Eemian and in the Holocene
that present some analogy in the Earth&apos;s orbital configuration in terms of
obliquity and precession. Simulations with the IPSL_CM4 ocean-atmosphere
coupled model allow us to discuss the response of the Indian and African
monsoon in terms of amplitude and response to the insolation forcing.
Results show that precession plays a large role in shaping the seasonal
timing of the monsoon system. Differences are found in the response of the
two sub-systems. They result from the phase relationship between the
insolation forcing and the seasonal characteristics of each sub-system. Also
the response of the Indian Ocean is very different in terms of temperature
and salinity when the change in insolation occurs at the summer solstice or
later in the year. Monsoon has a large contribution to heat and water
transports. It is shown that the relative importance of monsoon on the
change in the energetic of the tropical regions also vary with precession.</abstract>
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</article>

