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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>6</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acp-6-329-2006</doi>
	<article_url>http://www.atmos-chem-phys.net/6/329/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/6/329/2006/acp-6-329-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/6/329/2006/acp-6-329-2006.pdf</fulltext_pdf>
	<start_page>329</start_page>
	<end_page>338</end_page>
	<publication_date>2006-02-06</publication_date>
	<article_title content_type="html">Airborne multi-axis DOAS measurements of tropospheric SO&lt;sub&gt;2&lt;/sub&gt; plumes in the Po-valley, Italy</article_title>
	<authors>
		<author numeration="1" affiliations="1,4">
			<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>J. P. Burrows</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>R. Scheele</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>W. Junkermann</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>K.-P. Heue</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>T. Wagner</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>U. Platt</name>
		</author>
		<author numeration="10" affiliations="4">
			<name>I. Pundt</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">Royal Netherlands Meteorological Institute (KNMI), De Bilt, the Netherlands</affiliation>
		<affiliation numeration="3" content_type="html">Research Center Karlsruhe, IMK-IFU, Garmisch-Partenkirchen, Germany</affiliation>
		<affiliation numeration="4" content_type="html">Institute of Environmental Physics, University of Heidelberg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">During the second FORMAT (FORMaldehyde as A Tracer of oxidation in the troposphere)
campaign in 2003 the airborne multi-axis DOAS instrument (AMAXDOAS) performed
scattered-light spectroscopic measurements of SO&lt;sub&gt;2&lt;/sub&gt; over  the city of Mantova
and the power plant Porto Tolle, both situated in the Po-valley, Northern Italy.
The SO&lt;sub&gt;2&lt;/sub&gt; vertical columns and emission flux were derived from two days of
measurements, 26 and 27 September 2003. The SO&lt;sub&gt;2&lt;/sub&gt; emission flux from the power
plant Porto Tolle was calculated to 1.93&amp;times;10&lt;sup&gt;25&lt;/sup&gt; molec s&lt;sup&gt;-1&lt;/sup&gt; on
26 September and in good agreement with official emission data, which quote
2.25&amp;times;10&lt;sup&gt;25&lt;/sup&gt; molec s&lt;sup&gt;-1&lt;/sup&gt;. On 27 September the measured flux was
much lower (3.77&amp;times;10&lt;sup&gt;24&lt;/sup&gt; molec s&lt;sup&gt;-1&lt;/sup&gt;) if ECMWF wind data are used,
but of comparable magnitude (2.4&amp;times;10&lt;sup&gt;25&lt;/sup&gt; molec s&lt;sup&gt;-1&lt;/sup&gt;) if the
aircraft on-board wind measurements are utilised. Official emission
data was 2.07&amp;times;10&lt;sup&gt;25&lt;/sup&gt; molec s&lt;sup&gt;-1&lt;/sup&gt; indicating only a small
change from the previous day. Over the city of Mantova,
the observed SO&lt;sub&gt;2&lt;/sub&gt; vertical columns were 1.1&amp;times;10&lt;sup&gt;16&lt;/sup&gt; molec cm&lt;sup&gt;-2&lt;/sup&gt;
and 1.9&amp;times;10&lt;sup&gt;16&lt;/sup&gt; molec cm&lt;sup&gt;-2&lt;/sup&gt; on 26 and 27 September,
respectively. This is in good agreement with ground-based measurements
of 5.9 ppbv and 10.0 ppbv which correspond to
1.2&amp;times;10&lt;sup&gt;16&lt;/sup&gt; molec cm&lt;sup&gt;-2&lt;/sup&gt; and
2.2&amp;times;10&lt;sup&gt;16&lt;/sup&gt; molec cm&lt;sup&gt;-2&lt;/sup&gt; if a
well mixed boundary layer of 500m altitude is assumed.</abstract>
	<references>
	</references>
</article>

