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<!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>5</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-847-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/847/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/847/2005/acpd-5-847-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/847/2005/acpd-5-847-2005.pdf</fulltext_pdf>
	<start_page>847</start_page>
	<end_page>862</end_page>
	<publication_date>2005-02-16</publication_date>
	<article_title content_type="html">Shipborne solar absorption measurements of CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O and CO and comparison with SCIAMACHY WFM-DOAS retrievals</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. Warneke</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. de Beek</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Buchwitz</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Notholt</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>A. Schulz</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>V. Velazco</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>O. Schrems</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of environmental physics, University of Bremen, Bremen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Alfred Wegener Institute, Potsdam, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Alfred Wegener Institute, Bremerhaven, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">CO, CH&lt;sub&gt;4&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O and CO&lt;sub&gt;2&lt;/sub&gt; were retrieved from high resolution
solar absorption spectra obtained during a ship cruise from Capetown to
Bremerhaven in January/February 2003 by Fourier Transform Infrared (FTIR)
spectroscopy. Precisions of better than 0.5% for the column averaged
volume mixing ratios (VMR) of CH&lt;sub&gt;4&lt;/sub&gt; and CO&lt;sub&gt;2&lt;/sub&gt; are achieved using of
O&lt;sub&gt;2&lt;/sub&gt; as a reference gas. Shipborne FTIR-measurements of CO and data from
SCIAMACHY/ENVISAT retrieved by the Weighting Function Modified Differential
Optical Absorption Spectroscopy (WFM-DOAS) retrieval algorithm show
qualitatively the same latitudinal variations. WFM-DOAS data of CH&lt;sub&gt;4&lt;/sub&gt;,
N&lt;sub&gt;2&lt;/sub&gt;O and CO&lt;sub&gt;2&lt;/sub&gt; measured over sea exhibit a great spread. The spread
is significantly reduced for satellite measurements over land and a
reasonable agreement can be obtained if the shipborne data is compared with
the closest SCIAMACHY measurements over land. The number of comparisons is
too small to draw conclusions. However, by including only WFM-DOAS data with
small errors the shipborne and WFM-DOAS data compare within 5% for
CH&lt;sub&gt;4&lt;/sub&gt; and CO&lt;sub&gt;2&lt;/sub&gt; and within 30% for N&lt;sub&gt;2&lt;/sub&gt;O.</abstract>
	<references>
	</references>
</article>

