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<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>9</volume_number>
		<issue_number>11</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-3601-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/3601/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/3601/2009/acp-9-3601-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/3601/2009/acp-9-3601-2009.pdf</fulltext_pdf>
	<start_page>3601</start_page>
	<end_page>3612</end_page>
	<publication_date>2009-06-04</publication_date>
	<article_title content_type="html">Variability and trends in stratospheric NO&lt;sub&gt;2&lt;/sub&gt; in Antarctic summer, and implications for stratospheric NO&lt;sub&gt;y&lt;/sub&gt;</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. A. Cook</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. K. Roscoe</name>
			<email>hkro@bas.ac.uk</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">British Antarctic Survey, Madingley Rd, Cambridge CB3 0ET, UK</affiliation>
	</affiliations>
	<abstract content_type="html">NO&lt;sub&gt;2&lt;/sub&gt; measurements during 1990–2007, obtained from a zenith-sky
spectrometer in the Antarctic, are analysed to determine the long-term
changes in NO&lt;sub&gt;2&lt;/sub&gt;. An atmospheric photochemical box model and a radiative
transfer model are used to improve the accuracy of determination of the
vertical columns from the slant column measurements, and to deduce the
amount of NO&lt;sub&gt;y&lt;/sub&gt; from NO&lt;sub&gt;2&lt;/sub&gt;. We find that the NO&lt;sub&gt;2&lt;/sub&gt; and NO&lt;sub&gt;y&lt;/sub&gt; columns in
midsummer have large inter-annual variability superimposed on a broad
maximum in 2000, with little or no overall trend over the full time period.
These changes are robust to a variety of alternative settings when
determining vertical columns from slant columns or determining NO&lt;sub&gt;y&lt;/sub&gt; from
NO&lt;sub&gt;2&lt;/sub&gt;. They may signify similar changes in speed of the Brewer-Dobson
circulation but with opposite sign, i.e. a broad minimum around 2000.
Multiple regressions show significant correlation with solar and
quasi-biennial-oscillation indices, and weak correlation with El Nino, but
no significant overall trend, corresponding to an increase in Brewer-Dobson
circulation of 1.4&amp;plusmn;3.5%/decade. There remains an unexplained cycle
of amplitude and period at least 15% and 17 years, with minimum speed in
about 2000.</abstract>
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</article>

