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	<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>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-14169-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/14169/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/14169/2008/acpd-8-14169-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/14169/2008/acpd-8-14169-2008.pdf</fulltext_pdf>
	<start_page>14169</start_page>
	<end_page>14216</end_page>
	<publication_date>2008-07-23</publication_date>
	<article_title content_type="html">Measurement of the tropical UTLS composition in presence of clouds using millimetre-wave heterodyne spectroscopy</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>B. M. Dinelli</name>
			<email>bm.dinelli@isac.cnr.it</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>E. Castelli</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>B. Carli</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>S. Del Bianco</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. Gai</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>L. Santurri</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>B. P. Moyna</name>
		</author>
		<author numeration="8" affiliations="3">
			<name>M. Oldfield</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>R. Siddans</name>
		</author>
		<author numeration="10" affiliations="4">
			<name>D. Gerber</name>
		</author>
		<author numeration="11" affiliations="4">
			<name>W. J. Reburn</name>
		</author>
		<author numeration="12" affiliations="4">
			<name>B. J. Kerridge</name>
		</author>
		<author numeration="13" affiliations="5,6">
			<name>C. Keim</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Istituto di Scienze dell&apos;Atmosfera e del Clima – CNR, Bologna, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Istituto di Fisica Applicata &quot;N. Carrara&quot; – CNR, Florence, Italy</affiliation>
		<affiliation numeration="3" content_type="html">&quot;Millimetre-wave Technology Group&quot; RAL, Oxfordshire, UK</affiliation>
		<affiliation numeration="4" content_type="html">&quot;Remote Sensing Group&quot; RAL, Oxfordshire, UK</affiliation>
		<affiliation numeration="5" content_type="html">Institut für Meteorologie und Klimaforschung, Forschungszentrum Karlsruhe, Germany</affiliation>
		<affiliation numeration="6" content_type="html">now at: Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA) CNRS/Université de Paris 12 et 7, France</affiliation>
	</affiliations>
	<abstract content_type="html">The MARSCHALS (Millimetre-wave Airborne Receiver for Spectroscopic
CHaracterisation of Atmospheric Limb-Sounding) project has the general
objectives of demonstrating the measurement capabilities of a limb viewing
instrument working in the millimetre and sub-millimetre spectral regions for
the study of the Upper Troposphere – Lower Stratosphere (UTLS). MARSCHALS
has flown on board the M-55 stratospheric aircraft (Geophysica) in two
measurements campaigns. Here we report the results of the analysis of
MARSCHALS measurements during the SCOUT-O3 campaign held in Darwin
(Australia) in December 2005 obtained with MARC (Millimetre-wave
Atmospheric-Retrieval Code). MARSCHALS measured vertical distributions of
Temperature, water vapour, ozone and nitric acid. The retrieval has been
performed in the altitude range from 10 to 20 km in presence of clouds that
obscure measurements in the middle infrared spectroscopic region. The
minimum altitude range is determined by the high water concentration typical
of the tropical region rather than the extensive cloud coverage experienced
during the flight. The results have been validated using a few measurement
made in less cloudy conditions by MIPAS-STR, an infrared limb-viewing
instrument on board the M-55 during the same flight.</abstract>
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</article>

