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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-5-2311-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/2311/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/2311/2009/cpd-5-2311-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/2311/2009/cpd-5-2311-2009.pdf</fulltext_pdf>
	<start_page>2311</start_page>
	<end_page>2341</end_page>
	<publication_date>2009-10-13</publication_date>
	<article_title content_type="html">Effects of orbital forcing on atmosphere and ocean heat transports in Holocene and Eemian climate simulations with a comprehensive Earth system model</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>N. Fischer</name>
			<email>nils.fischer@zmaw.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Jungclaus</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Meteorology, Hamburg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">International Max Planck Research School for Earth System Modelling, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Orbital forcing does not only exert direct insolation effects but also
      alters climate indirectly through feedback mechanisms that modify
      atmosphere and ocean dynamics and meridional heat and moisture
      transfers. We investigate the regional effects of these changes by
      detailed analysis of atmosphere and ocean circulation and heat
      transports in a coupled atmosphere-ocean-sea ice-biosphere general
      circulation model (ECHAM5/JSBACH/MPI-OM). We perform long term quasi
      equilibrium simulations under pre-industrial, mid-Holocene (6000
      years before present â€“ yBP), and Eemian (125 000 yBP)
      orbital boundary conditions. Compared to pre-industrial climate,
      Eemian and Holocene temperatures show generally warmer conditions at
      higher and cooler conditions at lower latitudes. Changes in sea-ice
      cover, ocean heat transports, and atmospheric circulation patterns
      lead to pronounced regional heterogeneity. Over Europe, the warming is
      most pronounced over the north-eastern part in accordance with recent
      reconstructions for the Holocene. We attribute this warming to
      enhanced ocean circulation in the Nordic Seas and enhanced
      ocean-atmosphere heat flux over the Barents Shelf in conduction with
      retreat of sea ice and intensified winter storm tracks over northern
      Europe.</abstract>
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