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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-6-329-2006</article-id>
<title-group>
<article-title>Airborne multi-axis DOAS measurements of tropospheric SO&lt;sub&gt;2&lt;/sub&gt; plumes in the Po-valley, Italy</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wang</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Richter</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bruns</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Burrows</surname>
<given-names>J. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Scheele</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Junkermann</surname>
<given-names>W.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Heue</surname>
<given-names>K.-P.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wagner</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Platt</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pundt</surname>
<given-names>I.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics, University of Bremen, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Royal Netherlands Meteorological Institute (KNMI), De Bilt, the Netherlands</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Research Center Karlsruhe, IMK-IFU, Garmisch-Partenkirchen, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute of Environmental Physics, University of Heidelberg, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>06</day>
<month>02</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>2</issue>
<fpage>329</fpage>
<lpage>338</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/6/329/2006/acp-6-329-2006.html">This article is available from http://www.atmos-chem-phys.net/6/329/2006/acp-6-329-2006.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/6/329/2006/acp-6-329-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/6/329/2006/acp-6-329-2006.pdf</self-uri>
<abstract>
<p>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.</p>
</abstract>
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