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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>5</volume_number>
		<issue_number>11</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-2981-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/2981/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/2981/2005/acp-5-2981-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/2981/2005/acp-5-2981-2005.pdf</fulltext_pdf>
	<start_page>2981</start_page>
	<end_page>2987</end_page>
	<publication_date>2005-11-07</publication_date>
	<article_title content_type="html">UV radiation below an Arctic vortex with severe ozone depletion</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>B. M. Knudsen</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. Jønch-Sørensen</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. Eriksen</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>B. J. Johnsen</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>G. E. Bodeker</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Danish Meteorological Institute, Copenhagen, Denmark</affiliation>
		<affiliation numeration="2" content_type="html">Norwegian Radiation Protection Authority, Oslo, Norway</affiliation>
		<affiliation numeration="3" content_type="html">National Institute of Water and Atmospheric Research, Lauder, New Zealand</affiliation>
	</affiliations>
	<abstract content_type="html">The erythemally weighted (UV) irradiance below the severely depleted Arctic
vortices in spring 1996 and 1997 were substantially elevated. On average the
UV increased 36 and 33% relative to the 1979-1981 mean assuming clear
skies from day 80-100 in 1996 and 1997, respectively. On clear sky days
large regions of the Arctic experienced maximum UV increases exceeding 70
and 50% on single days in 1996 and 1997, respectively. A minor fraction
of these increases are not anthropogenic and have a dynamical origin as seen
by comparison to 1982, when hardly any ozone depletion is expected.</abstract>
	<references>
	</references>
</article>

