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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>2</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/acpd-2-1545-2002</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/2/1545/2002/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/2/1545/2002/acpd-2-1545-2002.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/2/1545/2002/acpd-2-1545-2002.pdf</fulltext_pdf>
	<start_page>1545</start_page>
	<end_page>1597</end_page>
	<publication_date>2002-10-15</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, RMS&amp;nbsp; &amp;lt; 20%).  In every case in which the chemical weather
      forecasts were primarily responsible for the flight plans, the targeted features were observed.  Two forecasted phenomena are
      discussed in detail: outflow from Asia observed in the Mediterranean upper troposphere during MINOS, and outflow from North America
      observed in the middle troposphere over northern Europe during CONTRACE.  It is shown that although such pollution plumes 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&amp;nbsp; &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>

