<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>4</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-8381-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/8381/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/8381/2004/acpd-4-8381-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/8381/2004/acpd-4-8381-2004.pdf</fulltext_pdf>
	<start_page>8381</start_page>
	<end_page>8423</end_page>
	<publication_date>2004-12-15</publication_date>
	<article_title content_type="html">SCIAMACHY validation by aircraft remote measurements: design, execution, and first results of the SCIA-VALUE mission</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Fix</name>
			<email>andreas.fix@dlr.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. Ehret</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. Flentje</name>
		</author>
		<author numeration="4" affiliations="1,6">
			<name>G. Poberaj</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. Gottwald</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>H. Finkenzeller</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>H. Bremer</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>M. Bruns</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>J. P. Burrows</name>
		</author>
		<author numeration="10" affiliations="4">
			<name>A. Kleinböhl</name>
		</author>
		<author numeration="11" affiliations="4">
			<name>H. Küllmann</name>
		</author>
		<author numeration="12" affiliations="4">
			<name>J. Kuttippurath</name>
		</author>
		<author numeration="13" affiliations="4">
			<name>A. Richter</name>
		</author>
		<author numeration="14" affiliations="4">
			<name>P. Wang</name>
		</author>
		<author numeration="15" affiliations="5">
			<name>K.-P. Heue</name>
		</author>
		<author numeration="16" affiliations="5">
			<name>U. Platt</name>
		</author>
		<author numeration="17" affiliations="5">
			<name>T. Wagner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut für Physik der Atmosphäre, DLR Oberpfaffenhofen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Deutsches Fernerkundungsdatenzentrum, DLR Oberpfaffenhofen, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Flugbetrieb, DLR Oberpfaffenhofen, Germany</affiliation>
		<affiliation numeration="4" content_type="html">Institut für Umweltphysik, Universität Bremen, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Institut für Umweltphysik, Universität Heidelberg, Germany</affiliation>
		<affiliation numeration="6" content_type="html">now at: Swiss Federal Institute of Technology Zurich, Institute of Quantum Electronics, Zurich, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">For the first time three different remote sensing instruments &amp;ndash; a
sub-millimeter radiometer, a differential optical absorption spectrometer in
the UV-visible spectral range, and a lidar &amp;ndash; were deployed aboard DLR&apos;s
meteorological research aircraft Falcon 20 to validate a large number of
SCIAMACHY level 2 and off-line data products such as O&lt;sub&gt;3&lt;/sub&gt;, NO&lt;sub&gt;2&lt;/sub&gt;,
N&lt;sub&gt;2&lt;/sub&gt;O, BrO, OClO, H&lt;sub&gt;2&lt;/sub&gt;O, aerosols, and clouds. Within two main
validation campaigns of the SCIA-VALUE mission (SCIAMACHY VALidation and
Utilization Experiment) extended latitudinal cross-sections stretching from
polar regions to the tropics as well as longitudinal cross sections at polar
latitudes at about 70&amp;deg; N and the equator have been generated. This
contribution gives an overview over the campaigns performed and reports on
the observation strategy for achieving the validation goals. We also
emphasize the synergetic use of the novel set of aircraft instrumentation
and the usefulness of this innovative suite of remote sensing instruments
for satellite validation.</abstract>
	<references>
	</references>
</article>

