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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>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cpd-4-585-2008</doi>
	<article_url>http://www.clim-past-discuss.net/4/585/2008/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/4/585/2008/cpd-4-585-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/4/585/2008/cpd-4-585-2008.pdf</fulltext_pdf>
	<start_page>585</start_page>
	<end_page>610</end_page>
	<publication_date>2008-05-16</publication_date>
	<article_title content_type="html">Anticyclonic atmospheric circulation as an analogue for the warm and dry mid-Holocene summer climate in central Scandinavia</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. Antonsson</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>D. Chen</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>H. Seppä</name>
			<email>heikki.seppa@helsinki.fi</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth Sciences, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden</affiliation>
		<affiliation numeration="2" content_type="html">Earth Sciences Centre, University of Gothenburg, P.O. Box 460, 405 30, Göteborg, Sweden</affiliation>
		<affiliation numeration="3" content_type="html">Department of Geology, P.O. Box 64, 00014, University of Helsinki, Helsinki, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">Climate reconstructions from central Scandinavia suggest that annual and
summer temperatures were rising during the early Holocene and reached their
maximum after 8000 cal yr BP. The period with highest temperatures was
characterized by increasingly low lake-levels and dry climate, with driest
and warmest conditions at about 7000 to 5000 cal yr BP. We compare the
reconstructed climate pattern with simulations of a climate model for the
last 9000 yr and show that the model, which is predominantly driven by
solar insolation patterns, fails to produce the reconstructed mid-Holocene
dry and warm period in Scandinavia. As an alternative explanation for the
reconstructed climate, we hypothesize that the trend from the moist early
Holocene towards dry and warm mid-Holocene was caused by a changing
atmospheric circulation pattern with a mid-Holocene dominance of summer-time
anticyclonic circulation. An extreme case of the anticyclonic conditions is
the persistent blocking high, an atmospheric pressure pattern that at
present often causes long spells of particularly dry and warm summer
weather, or &quot;Indian summers&quot;. The hypothesis is tested with daily
instrumental temperature and precipitation records in central Sweden and an
objective circulation classification based on surface air pressure over the
period 1900&amp;ndash;2002. It is concluded that the differences between the
precipitation and temperature climates under anticyclonic and
non-anticyclonic conditions are significant. Further, warm and dry
combination, as indicated by mid-Holocene reconstructions, is a typical
pattern under anticyclonic conditions. These results indicate that the
presented hypothesis for the mid-Holocene climate is likely valid.</abstract>
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