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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>2</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/amtd-2-2919-2009</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/2/2919/2009/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/2/2919/2009/amtd-2-2919-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/2/2919/2009/amtd-2-2919-2009.pdf</fulltext_pdf>
	<start_page>2919</start_page>
	<end_page>2982</end_page>
	<publication_date>2009-11-18</publication_date>
	<article_title content_type="html">Extending differential optical absorption spectroscopy for limb measurements in the UV</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Puķīte</name>
			<email>janis.pukite@mpch-mainz.mpg.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Kühl</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>T. Deutschmann</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>U. Platt</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>T. Wagner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Chemistry, J. J. Becher Weg 27, 55128 Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Environmental Physics, University of Heidelberg, Im Neuenheimer Feld 229, 69120 Heidelberg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Methods of UV/VIS absorption spectroscopy to determine the constituents in
the Earth&apos;s atmosphere from measurements of scattered light are often based
on the Beer-Lambert law, like e.g. Differential Optical Absorption
Spectroscopy (DOAS). Therefore they are strictly valid for weak absorptions
and narrow wavelength intervals (strictly only for monochromatic radiation).
For medium and strong absorption (e.g. along very long light-paths like in
limb geometry) the relation between the optical depth and the concentration
of an absorber is not linear anymore. As well, for large wavelength intervals
the wavelength dependent differences in the travelled light-paths become
important, especially in the UV, where the probability for scattering
increases strongly with decreasing wavelength.
&lt;br&gt;&lt;br&gt;
However, by taking into account these dependencies, the applicability of the
DOAS method can be extended also to cases with medium to strong absorptions
and for broader wavelength intervals.
&lt;br&gt;&lt;br&gt;
Common approaches for this correction are the so called air mass factor
modified (or extended) DOAS and the weighting function modified DOAS. These
approaches take into account the wavelength dependency of the slant column
densities (SCDs), but also require a-priori knowledge for the air mass factor
or the weighting function calculation by radiative transfer modelling.
&lt;br&gt;&lt;br&gt;
We describe an approach that considers the fitting results obtained from
DOAS, the SCDs, as a function of wavelength and vertical optical depth and
expands this function into a Taylor series of both quantities. The Taylor
coefficients are then applied as additional fitting parameters in the DOAS
analysis. Thus the variability of the SCD in the fit window is determined by
the retrieval itself.
&lt;br&gt;&lt;br&gt;
This new approach gives a description of the SCD that is as close to reality
as desired (depending on the order of the Taylor expansion), and is
independent from any assumptions or a-priori knowledge of the considered
absorbers.
&lt;br&gt;&lt;br&gt;
In case studies for simulated and measured spectra in the UV (332–357 nm),
we demonstrate the improvement by this approach for the retrieval of vertical
profiles of BrO from the SCIAMACHY limb observations. Compared to the
standard DOAS approach, the results for BrO obtained from the simulated
spectra are closer to the true profile, when applying the new method for the
SCDs of ozone. Also for the measured spectra the agreement with validation
measurements is improved significantly, especially for cases with strong
ozone absorption.
&lt;br&gt;&lt;br&gt;
While the focus of this article is on the improvement of the BrO profile
retrieval from the SCIAMACHY limb measurements, the novel approach may be
applied for a wide range of DOAS retrievals.</abstract>
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</article>

