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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>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cpd-4-271-2008</doi>
	<article_url>http://www.clim-past-discuss.net/4/271/2008/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/4/271/2008/cpd-4-271-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/4/271/2008/cpd-4-271-2008.pdf</fulltext_pdf>
	<start_page>271</start_page>
	<end_page>287</end_page>
	<publication_date>2008-03-04</publication_date>
	<article_title content_type="html">Shifts in early spring wind regime in North-East Europe (1955&amp;ndash;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, Estonia</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Cybernetics at Tallinn University of Technology, Estonia</affiliation>
	</affiliations>
	<abstract content_type="html">Changes of the winter-to-spring switch-time of the upper air flow regime at
850 and 500 hPa levels over the north-eastern Baltic Sea are analyzed based
on a data set extending until 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 as well
as the 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>

