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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>4</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-6067-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/6067/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/6067/2004/acpd-4-6067-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/6067/2004/acpd-4-6067-2004.pdf</fulltext_pdf>
	<start_page>6067</start_page>
	<end_page>6106</end_page>
	<publication_date>2004-09-29</publication_date>
	<article_title content_type="html">Iterative maximum a posteriori (IMAP)-DOAS for retrieval of strongly absorbing trace gases: Model studies for CH&lt;sub&gt;4&lt;/sub&gt; and CO&lt;sub&gt;2&lt;/sub&gt; retrieval from near infrared spectra of SCIAMACHY onboard ENVISAT</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Frankenberg</name>
			<email>cfranken@iup.uni-heidelberg.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>U. Platt</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. Wagner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Environmental Physics, Heidelberg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">In the past, differential optical absorption spectroscopy (DOAS) has
mostly been employed for trace gas retrieval in the UV/Vis spectral
region. New spectrometers such as SCIAMACHY onboard ENVISAT
 also provide near infrared channels and thus allow for the detection of
 greenhouse gases like CH&lt;sub&gt;4&lt;/sub&gt;, CO&lt;sub&gt;2&lt;/sub&gt;, or N&lt;sub&gt;2&lt;/sub&gt;O.
 However, modifications of the classical DOAS algorithm are necessary to account for the
idiosyncrasies of this spectral region, i.e. the temperature and
pressure dependence of the high resolution absorption lines.
Furthermore, understanding the sensitivity of the measurement of
these high resolution, strong absorption lines by means of a
non-ideal device, i.e. having finite spectral resolution, is of
special importance. This applies not only in the NIR, but can also
prove to be an issue for the UV/Vis spectral region.

&lt;br&gt;&lt;br&gt;
This paper presents a modified iterative maximum a posteriori-DOAS (IMAP-DOAS) algorithm based on optimal estimation
theory introduced to the remote sensing community by
Rodgers (1976). This method directly iterates the vertical column
densities of the absorbers of interest until the expected total
optical density fits the measurement. Although the discussion in
this paper lays emphasis on satellite retrieval, the basic
principles of the algorithm also hold for arbitrary measurement
geometries.

&lt;br&gt;&lt;br&gt;
For a quantitative test of this new approach and a comparison with
classical algorithms, it is applied to modelled spectra based on a
comprehensive set of atmospheric temperature and pressure profiles.
This analysis reveals that the sensitivity of measurement strongly
depends on the prevailing pressure-height. The IMAP-DOAS
algorithm properly accounts for the sensitivity of measurement on
pressure due to pressure broadening of the absorption lines. Thus,
biases in the retrieved vertical columns that would arise in
classical algorithms, are obviated. Here, we analyse and quantify
these systematic biases as well as errors due to variations in the
temperature and pressure profiles, which is indispensable for the
understanding of measurement precision and accuracy in the near
infrared as well as for future intercomparisons of retrieval
algorithms.</abstract>
	<references>
	</references>
</article>

