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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>8</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-10873-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/10873/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/10873/2008/acpd-8-10873-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/10873/2008/acpd-8-10873-2008.pdf</fulltext_pdf>
	<start_page>10873</start_page>
	<end_page>10911</end_page>
	<publication_date>2008-06-06</publication_date>
	<article_title content_type="html">Quantitative performance metrics for stratospheric-resolving   chemistry-climate models</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. W. Waugh</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>V. Eyring</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth and Planetary Science,   Johns Hopkins University, Baltimore, MD, USA</affiliation>
		<affiliation numeration="2" content_type="html">Deutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">A set of performance metrics is applied to stratospheric-resolving
  chemistry-climate models (CCMs) to quantify their ability to
  reproduce key processes relevant for stratospheric ozone.  The same
  metrics are used to assign a quantitative measure of performance
  (&quot;grade&quot;) to each model-observations comparison shown in
  Eyring et al. (2006).  A wide range of grades is obtained, both for
  different diagnostics applied to a single model and for the same
  diagnostic applied to different models, highlighting the wide range
  in ability of the CCMs to simulate key processes in the
  stratosphere.  No model scores high or low on all tests, but
  differences in the performance of models can be seen, especially for
  transport processes where several models get low grades on multiple
  tests. The grades are used to assign relative weights to the CCM
  projections of 21st century total ozone.
  However, only small differences are found between weighted
  and unweighted multi-model mean total ozone projections.
  This study raises several issues with the grading and weighting of
  CCMs that need further examination, but it does provide a framework
  that will enable quantification of model improvements and assignment
  of relative weights to the model projections.</abstract>
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</article>

