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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-5-1521-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/1521/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/1521/2009/cpd-5-1521-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/1521/2009/cpd-5-1521-2009.pdf</fulltext_pdf>
	<start_page>1521</start_page>
	<end_page>1552</end_page>
	<publication_date>2009-05-27</publication_date>
	<article_title content_type="html">Last nine-thousand years of temperature variability in Northern Europe</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Seppä</name>
			<email>heikki.seppa@helsinki.fi</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. E. Bjune</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>R. J. Telford</name>
		</author>
		<author numeration="4" affiliations="3,4">
			<name>H. J. B. Birks</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>S. Veski</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geology, P.O. Box 65, 00014, University of Helsinki, Helsinki, Finland</affiliation>
		<affiliation numeration="2" content_type="html">Bjerknes Centre for Climate Research, c/o Department of Biology, University of Bergen, Allégaten 41, 5007 Bergen, Norway</affiliation>
		<affiliation numeration="3" content_type="html">Department of Biology, University of Bergen, Allégaten 41, 5007 Bergen, Norway</affiliation>
		<affiliation numeration="4" content_type="html">Environmental Change Research Centre, University College London, Gower Street, London WC1E 6BT, UK</affiliation>
		<affiliation numeration="5" content_type="html">Institute of Geology, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia</affiliation>
	</affiliations>
	<abstract content_type="html">The threat of future global warming has generated a major
interest in quantifying past climate variability on centennial and
millennial time-scales. However, palaeoclimatological records are often
noisy and arguments about past variability are only possible if they are
based on reproducible features in several reliably dated datasets. Here we
focus on the last 9000 years, explore the results of 35 Holocene
pollen-based July mean and annual mean temperature reconstructions from
Northern Europe by stacking them to create summary curves, and compare them
with a high-resolution, summary chironomid-based temperature record and
other independent palaeoclimate records. The stacked records show that the
&quot;Holocene Thermal Maximum&quot; in the region dates to 8000 to 4800 cal yr BP and
that the &quot;8.2 event&quot; and the &quot;Little Ice Age&quot; at 500–100 cal yr BP are the
clearest cold episodes during the Holocene. In addition, a more detailed
analysis of the last 5000 years pinpoints centennial-scale climate
variability with cold anomalies at 3800–3000 and 500–100 cal yr BP,
a long, warmer period around 2000 cal yr BP, and a marked warming since the
mid 19th century. The colder (warmer) anomalies are associated with
increased (decreased) humidity over the Northern European mainland,
consistent with the modern high correlation between cold (warm) and humid
(dry) modes of summer weather in the region. A comparison with the key proxy
records reflecting the main forcing factors does not support the hypothesis
that solar variability is the cause of the late-Holocene centennial-scale
temperature changes. We suggest that the reconstructed anomalies are typical
of Northern Europe and their occurrence may be related to the oceanic and
atmospheric circulation variability in the North Atlantic–North-European
region.</abstract>
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</article>

