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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>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-607-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/607/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/607/2007/cpd-3-607-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/607/2007/cpd-3-607-2007.pdf</fulltext_pdf>
	<start_page>607</start_page>
	<end_page>630</end_page>
	<publication_date>2007-03-15</publication_date>
	<article_title content_type="html">Spatial distribution of Pleistocene/Holocene warming amplitudes in Northern Eurasia inferred from geothermal data</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Yu. Demezhko</name>
			<email>ddem54@inbox.ru</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. G. Ryvkin</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>V. I. Outkin</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>A. D. Duchkov</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>V. T. Balobaev</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Geophysics, UB RAS, Ekaterinburg, Russia</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Geophysics, SB RAS, Novosibirsk, Russia</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Permafrost Studies, SB RAS, Yakutsk, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">We analyze 48 geothermal estimates of Pleistocene/Holocene warming amplitude
from various locations in Greenland, Europe, Arctic regions of Western
Siberia, and Yakutia. The spatial distribution of these estimates exhibits
two remarkable features. (i) In Europe and part of Asia the amplitude of
warming increases towards northwest and displays clear asymmetry with
respect to the North Pole. The region of maximal warming is close to the
North Atlantic. A simple parametric dependence of the amplitude on the
distance to the warming center explains 91% of the amplitude variation.
The Pleistocene/Holocene warming center is located northeast of Iceland. We
claim that the Holocene warming is primarily related to the formation (or
resumption) of the modern system of currents in the North Atlantic. (ii) In
Arctic Asia, north of the 68-th parallel, the amplitude sharply decreases
from South to North, reaching zero and even negative values. Too small
amplitudes could be attributed to a joint warming influence of Late
Pleistocene ice sheets and warm-water lakes formed in Late Pleistocene by
the damming of the Ob, Yenisei and Lena Rivers. Using a simple model of the
temperature regime underneath the ice sheet we show that, depending on the
relationship between the heat flow and the vertical ice advection velocity,
the base of the glacier can either warm up or cool down.</abstract>
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</article>

