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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>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acp-3-267-2003</doi>
	<article_url>http://www.atmos-chem-phys.net/3/267/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/3/267/2003/acp-3-267-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/3/267/2003/acp-3-267-2003.pdf</fulltext_pdf>
	<start_page>267</start_page>
	<end_page>289</end_page>
	<publication_date>2003-02-26</publication_date>
	<article_title content_type="html">Global chemical weather forecasts for field campaign planning: predictions and observations of large-scale features during MINOS, CONTRACE, and INDOEX</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. G. Lawrence</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>P. J. Rasch</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. von Kuhlmann</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Williams</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>H. Fischer</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. de Reus</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>J. Lelieveld</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>P. J. Crutzen</name>
		</author>
		<author numeration="9" affiliations="3">
			<name>M. Schultz</name>
		</author>
		<author numeration="10" affiliations="3">
			<name>P. Stier</name>
		</author>
		<author numeration="11" affiliations="4">
			<name>H. Huntrieser</name>
		</author>
		<author numeration="12" affiliations="4">
			<name>J. Heland</name>
		</author>
		<author numeration="13" affiliations="5">
			<name>A. Stohl</name>
		</author>
		<author numeration="14" affiliations="5">
			<name>C. Forster</name>
		</author>
		<author numeration="15" affiliations="6">
			<name>H. Elbern</name>
		</author>
		<author numeration="16" affiliations="6">
			<name>H. Jakobs</name>
		</author>
		<author numeration="17" affiliations="7">
			<name>R. R. Dickerson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max-Planck-Institut für Chemie, Postfach 3060, 55020 Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">National Center for Atmospheric Research, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">Max-Planck-Institut für Meteorologie, Hamburg, Germany</affiliation>
		<affiliation numeration="4" content_type="html">Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Technische Universität München, München, Germany</affiliation>
		<affiliation numeration="6" content_type="html">Institut für Geophysik und Meteorologie, Universität zu Köln, Köln, Germany</affiliation>
		<affiliation numeration="7" content_type="html">Department of Meteorology, University of Maryland, College Park, Maryland, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The first global tropospheric forecasts of
      O&lt;sub&gt;3&lt;/sub&gt; and its precursors have been used in the daily flight planning of field measurement
      campaigns.  The 3-D chemistry-transport model MATCH-MPIC is driven by meteorological data from a weather center (NCEP) to produce daily
      3-day forecasts of the global distributions of O&lt;sub&gt;3&lt;/sub&gt;

       and related
      gases, as well as regional CO tracers.  This paper describes the forecast system and its use in three field campaigns, MINOS, CONTRACE
      and INDOEX.  An overview is given of the forecasts by MATCH-MPIC and by three other chemical weather forecast models
      (EURAD, ECHAM, and FLEXPART), focusing on O&lt;sub&gt;3&lt;/sub&gt;

       and CO.  Total CO and regional CO tracers
      were found to be the most valuable gases for flight planning, due to their relatively well-defined anthropogenic source regions and
      lifetimes of one to a few months.  CO was in good agreement with the observations on nearly all the flights (generally&amp;nbsp;
      r &amp;gt; 0.7, and the relative RMS differences for the deviations from the means was less
      than 20%).  In every case in which the chemical weather forecasts were primarily responsible for the flight plans, the targeted features
      were observed.  Three forecasted phenomena are discussed in detail: outflow from Asia observed in the Mediterranean upper troposphere
      during MINOS, outflow from North America observed in the middle troposphere over northern Europe during CONTRACE, and the location of
      the &amp;quot;chemical ITCZ&apos;&apos; over the Indian Ocean during INDOEX.  In particular it is shown that although intercontinental pollution plumes
      such as those observed during MINOS and CONTRACE occur repeatedly during the months around the campaigns, their frequency is
      sufficiently low (~10--30% of the time) that global chemical weather forecasts are important for enabling them to be observed
      during limited-duration field campaigns.  The MATCH-MPIC chemical weather forecasts, including an interface for making customized
      figures from the output, are available for community use via &lt;a href=&quot;http://www.mpch-mainz.mpg.de/~lawrence/forecasts.html&quot;&gt;http://www.mpch-mainz.mpg.de/~lawrence/forecasts.html&lt;/a&gt;.</abstract>
	<references>
	</references>
</article>

