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	<journal>
		<journal_title>Climate of the Past</journal_title>
		<journal_url>www.clim-past.net</journal_url>
		<issn>1814-9324</issn>
		<eissn>1814-9332</eissn>
		<volume_number>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cp-4-147-2008</doi>
	<article_url>http://www.clim-past.net/4/147/2008/</article_url>
	<abstract_html>http://www.clim-past.net/4/147/2008/cp-4-147-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/4/147/2008/cp-4-147-2008.pdf</fulltext_pdf>
	<start_page>147</start_page>
	<end_page>152</end_page>
	<publication_date>2008-08-04</publication_date>
	<article_title content_type="html">Shifts in early spring wind regime in North-East Europe (1955–2007)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Keevallik</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>T. Soomere</name>
			<email>soomere@cs.ioc.ee</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Marine Systems Institute at Tallinn University of Technology, Akadeemia tee 21, 12618, Estonia</affiliation>
		<affiliation numeration="2" content_type="html">Centre for Nonlinear Studies, Institute of Cybernetics at Tallinn University of Technology, Akadeemia tee 21, 12618, Estonia</affiliation>
	</affiliations>
	<abstract content_type="html">Changes to the winter-to-spring switch-time of the upper air flow regime at
the 850 and 500 hPa levels over the north-eastern Baltic Sea are analyzed
based on a data set extending from 1955 to 2007. The long-term variation of
the air flow in early spring (March) exhibits multiple regime shifts. The
shifts are extracted by means of a vector analysis of the monthly mean air
flow and using statistical shift detection technology. In the middle of the
1960s the average air flow turned from NW (WNW) to W (WSW) at the 500 (850) hPa
level. The original regime was restored in the mid-1990s. The regime
shifts in the average air flow in March can be interpreted as changes in the
transition time from winter to summer circulation type.</abstract>
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</article>

