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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>7</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-9561-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/9561/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/9561/2007/acpd-7-9561-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/9561/2007/acpd-7-9561-2007.pdf</fulltext_pdf>
	<start_page>9561</start_page>
	<end_page>9633</end_page>
	<publication_date>2007-07-04</publication_date>
	<article_title content_type="html">Data assimilation of stratospheric constituents: a review</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>W. A. Lahoz</name>
			<email>swslahoz@rdg.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>Q. Errera</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>R. Swinbank</name>
		</author>
		<author numeration="4" affiliations="2,4">
			<name>D. Fonteyn</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Data Assimilation Research Centre, University of Reading, UK</affiliation>
		<affiliation numeration="2" content_type="html">BIRA-IASB, Brussels, Belgium</affiliation>
		<affiliation numeration="3" content_type="html">Met Office, Exeter, UK</affiliation>
		<affiliation numeration="4" content_type="html">now at: Belgian Federal Science Office, Belgium</affiliation>
	</affiliations>
	<abstract content_type="html">The data assimilation of stratospheric constituents is reviewed. The data
assimilation method is introduced, with particular consideration to its
application to stratospheric constituent measurements. Differences from
meteorological data assimilation are outlined. Historically, two approaches
have been used to carry out constituent assimilation. One approach has
carried constituent assimilation out as part of a numerical weather
prediction system; the other has carried it out in a standalone chemical
model, often with a more sophisticated representation of chemical processes.
Whereas the aim of the numerical weather prediction approach has been to
improve weather forecasts, the aims of the chemical model approach have
included providing chemical forecasts and analyses of chemical constituents.
A range of constituent assimilation systems developed in these two areas is
presented and strengths and weaknesses discussed. The use of stratospheric
constituent data assimilation to evaluate models, observations and analyses,
and to provide analyses of constituents, monitor ozone, and make ozone
forecasts is discussed. Finally, the current state of affairs is assessed,
future directions are discussed, and potential key drivers identified.</abstract>
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</article>

