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<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>7</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-7907-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/7907/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/7907/2007/acpd-7-7907-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/7907/2007/acpd-7-7907-2007.pdf</fulltext_pdf>
	<start_page>7907</start_page>
	<end_page>7932</end_page>
	<publication_date>2007-06-04</publication_date>
	<article_title content_type="html">ACE-FTS observation of a young biomass burning plume: first reported measurements of C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;4&lt;/sub&gt;, C&lt;sub&gt;3&lt;/sub&gt;H&lt;sub&gt;6&lt;/sub&gt;O, H&lt;sub&gt;2&lt;/sub&gt;CO and PAN by infrared occultation from space</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P.-F. Coheur</name>
			<email>pfcoheur@ulb.ac.be</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. Herbin</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>C. Clerbaux</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>D. Hurtmans</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>C. Wespes</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. Carleer</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>S. Turquety</name>
		</author>
		<author numeration="8" affiliations="3">
			<name>C. P. Rinsland</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>J. Remedios</name>
		</author>
		<author numeration="10" affiliations="5">
			<name>D. Hauglustaine</name>
		</author>
		<author numeration="11" affiliations="6">
			<name>C. D. Boone</name>
		</author>
		<author numeration="12" affiliations="6,7">
			<name>P. F. Bernath</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Spectroscopie de l&apos;atmosphère, Chimie Quantique et Photophysique, Université Libre de Bruxelles (U.L.B.), Brussels, Belgium</affiliation>
		<affiliation numeration="2" content_type="html">Service d&apos;Aéronomie/Institut Pierre-Simon Laplace, CNRS, Université Pierre et Marie Curie-Paris6, France</affiliation>
		<affiliation numeration="3" content_type="html">NASA Langley Research Center, Mail Stop 401A, Hampton, VA 23681-2199, USA</affiliation>
		<affiliation numeration="4" content_type="html">Earth Observation Science, Space Research Centre, Department of Physics &amp; Astronomy University of Leicester, University Road, Leicester, LE1 7RH, UK</affiliation>
		<affiliation numeration="5" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environnement (LSCE)/Institut Pierre-Simon Laplace, CEA-CNRS, F-91191 Gif-sur-Yvette CEDEX, France</affiliation>
		<affiliation numeration="6" content_type="html">Department of Chemistry, University of Waterloo, Waterloo, Ontario, N2L 3G1, Canada</affiliation>
		<affiliation numeration="7" content_type="html">Department of Chemistry, University of York, Heslington, York YO10 5DD, UK</affiliation>
	</affiliations>
	<abstract content_type="html">In the course of our study of the upper tropospheric composition with the
infrared Atmospheric Chemistry Experiment &amp;ndash; Fourier Transform Spectrometer
(ACE&amp;ndash;FTS), we found an occultation sequence that on 8 October 2005, sampled
a remarkable plume near the east coast of Tanzania. Model simulations of the
CO distribution in the Southern hemisphere are performed for this period and
they demonstrate that the emissions for this event originated from a nearby
forest fire, after which the plume was transported from the source region to
the upper troposphere. Taking advantage of the very high signal-to-noise
ratio of the ACE&amp;ndash;FTS spectra over a wide wavenumber range (750&amp;ndash;4400 cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;), we present in-depth analyses of the chemical composition of this
plume in the middle and upper troposphere, focusing on the measurements of
weakly absorbing pollutants. For this specific biomass burning event, we
report simultaneous observations of an unprecedented number of organic
species. Measurements of C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;4&lt;/sub&gt; (ethene), C&lt;sub&gt;3&lt;/sub&gt;H&lt;sub&gt;4&lt;/sub&gt; (propyne),
H&lt;sub&gt;2&lt;/sub&gt;CO (formaldehyde), C&lt;sub&gt;3&lt;/sub&gt;H&lt;sub&gt;6&lt;/sub&gt;O (acetone) and
CH&lt;sub&gt;3&lt;/sub&gt;COO&lt;sub&gt;2&lt;/sub&gt;NO&lt;sub&gt;2&lt;/sub&gt; (peroxyacetylnitrate, abbreviated as PAN) are the
first reported detections using infrared occultation spectroscopy from
satellites. Based on the lifetime of the emitted species, we discuss the
photochemical age of the plume and also report, whenever possible, the
enhancement ratios relative to CO.</abstract>
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</article>

