<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-7-283-2007</article-id>
<title-group>
<article-title>Measurements of O&lt;sub&gt;3&lt;/sub&gt;, NO&lt;sub&gt;2&lt;/sub&gt; and BrO during the INDOEX campaign using ground based DOAS and GOME satellite data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ladstätter-Weißenmayer</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>Altmeyer</surname>
<given-names>H.</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>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>Rozanov</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>Rozanov</surname>
<given-names>V.</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>Wittrock</surname>
<given-names>F.</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-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics, University of Bremen, P.O. Box 330440, D-28334 Bremen, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>01</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>2</issue>
<fpage>283</fpage>
<lpage>291</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/7/283/2007/acp-7-283-2007.html">This article is available from http://www.atmos-chem-phys.net/7/283/2007/acp-7-283-2007.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/7/283/2007/acp-7-283-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/283/2007/acp-7-283-2007.pdf</self-uri>
<abstract>
<p>The INDian Ocean EXperiment (INDOEX) was an
international, multi-platform field campaign to measure long-range
transport of air masses from South and South-East-(SE) Asia
towards the Indian Ocean. During the dry monsoon season between
January and March 1999, local measurements were carried out from
ground based platforms and were compared with satellite based
data. The objective of this study was to characterise
stratospheric and tropospheric trace gas amounts in the equatorial
region, and to investigate the impact of air pollution at this
remote site. For the characterisation of the chemical composition
of the outflow from the S-SE-Asian region, we performed ground
based dual-axis-DOAS (Differential Optical Absorption
Spectroscopy) measurements at the KCO (Kaashidhoo Climate
Observatory) in the Maldives (5.0&amp;deg; N,
73.5&amp;deg; E). The measurements were conducted using two
different observation modes (off-axis and zenith-sky). This
technique allows the separation of the tropospheric and
stratospheric columns for different trace gases like O&lt;sub&gt;3&lt;/sub&gt;
and NO&lt;sub&gt;2&lt;/sub&gt;. These dual-axis DOAS data were compared with
O&lt;sub&gt;3&lt;/sub&gt;-sonde measurements performed at KCO and satellite based
GOME (Global Ozone Measuring Experiment) data during the intensive
measuring phase of the INDOEX campaign in February and March 1999.
From GOME observations, tropospheric and stratospheric columns for
O&lt;sub&gt;3&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt; were retrieved. In addition, the
analysis of the O&lt;sub&gt;3&lt;/sub&gt;-sonde measurements allowed the
determination of the tropospheric O&lt;sub&gt;3&lt;/sub&gt; amount. The
comparison shows that the results of all three measurement systems
agree within their error limits. During the INDOEX campaign,
mainly background conditions were observed, but in a single case
an increase of tropospheric NO&lt;sub&gt;2&lt;/sub&gt; during a short pollution
event was observed from the ground and the impact on the vertical
columns was calculated. GOME measurements showed evidence for
small tropospheric contributions to the BrO budget,
probably located in the free troposphere and present over long
periods of the year. The amounts of  BrO have been
investigated by the comparison of satellite pixels influenced by
high and low cloud conditions based on GOME data which allows the
determination of the detection limit of
3.8&amp;times;10&lt;sup&gt;13&lt;/sup&gt;molecules cm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; of tropospheric BrO
columns.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>