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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>6</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-9273-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/9273/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/9273/2006/acpd-6-9273-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/9273/2006/acpd-6-9273-2006.pdf</fulltext_pdf>
	<start_page>9273</start_page>
	<end_page>9296</end_page>
	<publication_date>2006-09-26</publication_date>
	<article_title content_type="html">Measurements of O&lt;ub&gt;3&lt;/sub&gt;, NO&lt;sub&gt;2&lt;/sub&gt; and BrO at the Kaashidhoo Climate Observatory (KCO) during the INDOEX (INDian Ocean EXperiment) Campaign using ground based DOAS (Differential Optical Absorption Spectroscopy) and satellite based GOME (Global Ozone Monitoring Experiment) data</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Ladstätter-Weißenmayer</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. Altmeyer</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Bruns</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>A. Richter</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>A. Rozanov</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>V. Rozanov</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>F. Wittrock</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>J. P. Burrows</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Environmental Physics, University of Bremen, P.O. Box 330440, 28334 Bremen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">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 ground based dual-axis-DOAS 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, background conditions were observed most of
the time, but in a single case an increase of tropospheric
NO&lt;sub&gt;2&lt;/sub&gt; during a short pollution event was observed and the
impact on the vertical columns was calculated. In the GOME
measurements, evidence was found for large tropospheric
contributions to the BrO budget, probably located in the
free troposphere and present throughout the year. The latter has
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 tropospheric
BrO columns.</abstract>
	<references>
	</references>
</article>

