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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>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-1297-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/1297/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/1297/2009/cpd-5-1297-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/1297/2009/cpd-5-1297-2009.pdf</fulltext_pdf>
	<start_page>1297</start_page>
	<end_page>1336</end_page>
	<publication_date>2009-05-05</publication_date>
	<article_title content_type="html">Warm Paleocene/Eocene climate as simulated in ECHAM5/MPI-OM</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>M. Heinemann</name>
			<email>malte.heinemann@zmaw.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. H. Jungclaus</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. Marotzke</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Meteorology (MPI-M), Hamburg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">International Max Planck Research School on Earth System Modelling (IMPRS-ESM), Hamburg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">We investigate the late Paleocene/early Eocene (PE) climate using the
coupled atmosphere-ocean-sea ice model ECHAM5/MPI-OM. The surface in our PE
control simulation is on average 297 K warm and ice-free, despite a moderate
CO&lt;sub&gt;2&lt;/sub&gt; concentration of 560 ppm. Compared to a pre-industrial reference
simulation (PR), low latitudes are 5 to 8 K warmer, while high latitudes are
up to 40 K warmer. This high-latitude amplification is in line with proxy
data, yet a comparison to sea surface temperature proxy data suggests that
the Arctic surface temperatures are still too low.

&lt;br&gt;&lt;br&gt;

To identify the mechanisms that cause the PE-PR temperature difference, we
fit a zero-dimensional energy balance model to the ECHAM5/MPI-OM results.
Doubled &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; in PE compared to PR, increased atmospheric water vapour, and
a slightly increased longwave cloud radiative forcing together cause about
2/3 of the PE-PR temperature difference; planetary albedo changes cause about
1/3. Our results support the hypothesis that local radiative effects as well
as topographic changes, rather than increased meridional heat transports,
were responsible for the &quot;equable&quot; PE climate.</abstract>
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