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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>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-323-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/323/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/323/2003/acpd-3-323-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/323/2003/acpd-3-323-2003.pdf</fulltext_pdf>
	<start_page>323</start_page>
	<end_page>353</end_page>
	<publication_date>2003-01-29</publication_date>
	<article_title content_type="html">A fast H&lt;sub&gt;2&lt;/sub&gt;O total column density product from GOME &amp;ndash; validation with in-situ aircraft measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. Wagner</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. Heland</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>M. Zöger</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>U. Platt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut für Umweltphysik, University of Heidelberg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">2Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany</affiliation>
		<affiliation numeration="3" content_type="html">3Deutsches Zentrum für Luft- und Raumfahrt (DLR), Flugabteilung, Oberpfaffenhofen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Atmospheric water vapour is the most important greenhouse gas which is responsible for
      about 2/3 of the natural greenhouse effect, therefore changes in atmospheric water vapour in a
      changing climate (the water vapour feedback) is subject to intense debate.
      H&lt;sub&gt;2&lt;/sub&gt;O is also involved in many important reaction cycles of atmospheric chemistry, e.g. in the production of
      the OH radical. Thus, long time series of global H&lt;sub&gt;2&lt;/sub&gt;O data are highly required. Since 1995 the
      Global Ozone Monitoring Experiment (GOME) continuously observes atmospheric trace
      gases. In particular it has been demonstrated that GOME as a nadir looking
      UV/vis-instrument is sensitive to many tropospheric trace gases. Here we present a new, fast
      H&lt;sub&gt;2&lt;/sub&gt;O algorithm for the retrieval of vertical column densities from GOME measurements. In contrast to existing
      H&lt;sub&gt;2&lt;/sub&gt;O retrieval algorithms it does not depend on additional information like e.g. the climatic
      zone, aerosol content or ground albedo. It includes an internal cloud-, aerosol-, and albedo
      correction which is based on simultaneous observations of the oxygen dimer
      O&lt;sub&gt;4&lt;/sub&gt;. The high accuracy of our GOME H&lt;sub&gt;2&lt;/sub&gt;O data is confirmed by the excellent agreement with in-situ aircraft
      measurements during the MINOS campaign in Greece in summer 2001. Our H&lt;sub&gt;2&lt;/sub&gt;O algorithm
      can be directly adapted to the nadir observations of SCIAMACHY (SCanning Imaging
      Absorption SpectroMeter for Atmospheric CHartographY) which was launched on ENVISAT
      in March 2002. Near real time H&lt;sub&gt;2&lt;/sub&gt;O column data from GOME and SCIAMACHY might be of
      great value for meteorological weather forecast.</abstract>
	<references>
	</references>
</article>

