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<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>7</volume_number>
		<issue_number>23</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acp-7-5971-2007</doi>
	<article_url>http://www.atmos-chem-phys.net/7/5971/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/7/5971/2007/acp-7-5971-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/7/5971/2007/acp-7-5971-2007.pdf</fulltext_pdf>
	<start_page>5971</start_page>
	<end_page>5987</end_page>
	<publication_date>2007-12-07</publication_date>
	<article_title content_type="html">SCIAMACHY tropospheric NO&lt;sub&gt;2&lt;/sub&gt; over Switzerland: estimates of NO&lt;sub&gt;x&lt;/sub&gt; lifetimes and impact of the complex Alpine topography on the retrieval</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Schaub</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. Brunner</name>
			<email>dominik.brunner@empa.ch</email>
		</author>
		<author numeration="3" affiliations="2">
			<name>K. F. Boersma</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>J. Keller</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>D. Folini</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>B. Buchmann</name>
		</author>
		<author numeration="7" affiliations="4,6">
			<name>H. Berresheim</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>J. Staehelin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Empa, Swiss Federal Laboratories for Materials Testing and Research, Ueberlandstrasse 129, 8600 Duebendorf, Switzerland</affiliation>
		<affiliation numeration="2" content_type="html">School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USA</affiliation>
		<affiliation numeration="3" content_type="html">Paul Scherrer Institute (PSI), 5232 Villigen PSI, Switzerland</affiliation>
		<affiliation numeration="4" content_type="html">German National Meteorological Service, DWD/MOHp, 82383 Hohenpeissenberg, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Swiss Federal Institute of Technology (ETH), Universitätstrasse 16, 8092 Zurich, Switzerland</affiliation>
		<affiliation numeration="6" content_type="html">now at: National University of Ireland Galway, Department of Physics, University Road, Galway, Ireland</affiliation>
	</affiliations>
	<abstract content_type="html">This study evaluates NO&lt;sub&gt;2&lt;/sub&gt; vertical tropospheric column
densities (VTCs) retrieved from measurements of the Scanning
Imaging Absorption Spectrometer for Atmospheric Chartography
(SCIAMACHY) above Switzerland and the Alpine region. The close
correlation between pixel averaged NO&lt;sub&gt;x&lt;/sub&gt; emission rates
from a spatially and temporally highly resolved inventory and the
NO&lt;sub&gt;2&lt;/sub&gt; VTCs under anticyclonic meteorological conditions
demonstrates the general ability of SCIAMACHY to detect sources of
NO&lt;sub&gt;x&lt;/sub&gt; pollution in Switzerland. This correlation is further
used to infer seasonal mean NO&lt;sub&gt;x&lt;/sub&gt; lifetimes carefully
taking into account the influence of the strong diurnal cycle in
NO&lt;sub&gt;x&lt;/sub&gt; emissions on these estimates. Lifetimes are estimated
to 3.6 (&amp;plusmn;0.8) hours in summer and 13.1 (&amp;plusmn;3.8) hours in
winter, the winter value being somewhat lower than previous
estimates. A comparison between the 2003-2005 mean NO&lt;sub&gt;2&lt;/sub&gt; VTC
distribution over Switzerland and the corresponding 1996&amp;ndash;2003 mean
from the Global Ozone Monitoring Experiment (GOME) illustrates the
much better capability of SCIAMACHY to resolve regional scale
pollution features. However, the comparison of seasonal averages
over the Swiss Plateau with GOME and ground based in situ
observations indicates that SCIAMACHY exhibits a too weak seasonal
cycle with comparatively high values in summer and low values in
winter. A problem likely contributing to the reduced values in
winter (not reported in earlier literature) is the use of
inaccurate satellite pixel surface pressures derived from a coarse
resolution global model in the retrieval. The marked topography in
the Alpine region can lead to deviations of several hundred meters
between the model assumed and the real pixel-averaged surface
height. A sensitivity study based on selected clear sky SCIAMACHY
NO&lt;sub&gt;2&lt;/sub&gt; VTCs over the Swiss Plateau and two fixed a priori
NO&lt;sub&gt;2&lt;/sub&gt; profile shapes indicates that inaccurate pixel surface
pressures affect retrieved NO&lt;sub&gt;2&lt;/sub&gt; columns over complex terrain by
up to 40%. For retrievals in the UV-visible spectral range with a
decreasing sensitivity towards the earth&apos;s surface, this effect is
of major importance when the NO&lt;sub&gt;2&lt;/sub&gt; resides close to the ground,
a situation most frequently observed during winter.</abstract>
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