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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<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>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-337-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/337/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/337/2005/acp-5-337-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/337/2005/acp-5-337-2005.pdf</fulltext_pdf>
	<start_page>337</start_page>
	<end_page>343</end_page>
	<publication_date>2005-02-07</publication_date>
	<article_title content_type="html">Measurements of tropospheric NO&lt;sub&gt;2&lt;/sub&gt; with an airborne multi-axis DOAS instrument</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Wang</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Richter</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Bruns</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>V. V. Rozanov</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. P. Burrows</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>K.-P. Heue</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>T. Wagner</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>I. Pundt</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>U. Platt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Environmental Physics, University of Bremen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Environmental Physics, University of Heidelberg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The AMAXDOAS instrument is an airborne multi-axis DOAS instrument
covering the spectral range from 300 to 600&amp;nbsp;nm. During one
flight of the SCIAVALUE campaign on 19 March 2003, the AMAXDOAS
onboard the DLR Falcon detected tropospheric NO&lt;sub&gt;2&lt;/sub&gt; over
Europe under both cloudy and cloud free conditions. By combining
the measurements in nadir and zenith direction, and analysing the
spectra in the UV and the visible spectral region, information was
derived on where the bulk of the observed NO&lt;sub&gt;2&lt;/sub&gt; was located.
Vertical columns of up to 5.7x10&lt;sup&gt;16&lt;/sup&gt; molec&amp;nbsp;cm&lt;sup&gt;-2&lt;/sup&gt; were observed close to Frankfurt, with a
distribution peaking in the boundary layer and in good agreement
with surface measurements. On several occasions, strong
tropospheric NO&lt;sub&gt;2&lt;/sub&gt; signals were also detected when flying
above clouds. The ratio of zenith and nadir measurements indicates
that the NO&lt;sub&gt;2&lt;/sub&gt; observed was located within the cloud, and
assuming the same profile as for the cloud free situation the
NO&lt;sub&gt;2&lt;/sub&gt; vertical column was estimated to be 5.0x10&lt;sup&gt;16&lt;/sup&gt; molec&amp;nbsp;cm&lt;sup&gt;-2&lt;/sup&gt;. The results are relevant for the
retrieval of tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns from space-borne
instruments in cloudy situations.</abstract>
	<references>
	</references>
</article>

