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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>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-727-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/727/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/727/2008/acpd-8-727-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/727/2008/acpd-8-727-2008.pdf</fulltext_pdf>
	<start_page>727</start_page>
	<end_page>779</end_page>
	<publication_date>2008-01-11</publication_date>
	<article_title content_type="html">Technical Note: Validation of Odin/SMR limb observations of ozone, comparisons with  OSIRIS, POAM III, ground-based and balloon-borne instruments</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>F. JÃ©gou</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. Urban</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>J. de La NoÃ«</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>P. Ricaud</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>E. Le FlochmoÃ«n</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>D. P. Murtagh</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>P. Eriksson</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>A. Jones</name>
		</author>
		<author numeration="9" affiliations="5,14">
			<name>S. Petelina</name>
		</author>
		<author numeration="10" affiliations="5">
			<name>E. J. Llewellyn</name>
		</author>
		<author numeration="11" affiliations="5">
			<name>N. D. Lloyd</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>C. Haley</name>
		</author>
		<author numeration="13" affiliations="7">
			<name>J. Lumpe</name>
		</author>
		<author numeration="14" affiliations="8">
			<name>C. Randall</name>
		</author>
		<author numeration="15" affiliations="9">
			<name>R. M. Bevilacqua</name>
		</author>
		<author numeration="16" affiliations="10">
			<name>V. Catoire</name>
		</author>
		<author numeration="17" affiliations="10">
			<name>N. Huret</name>
		</author>
		<author numeration="18" affiliations="10">
			<name>G. Berthet</name>
		</author>
		<author numeration="19" affiliations="10">
			<name>J. B. Renard</name>
		</author>
		<author numeration="20" affiliations="11">
			<name>K. Strong</name>
		</author>
		<author numeration="21" affiliations="12">
			<name>J. Davies</name>
		</author>
		<author numeration="22" affiliations="12">
			<name>C. T. Mc Elroy</name>
		</author>
		<author numeration="23" affiliations="13">
			<name>F. Goutail</name>
		</author>
		<author numeration="24" affiliations="13">
			<name>J. P. Pommereau</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environnement, Gif sur Yvette, France</affiliation>
		<affiliation numeration="2" content_type="html">Chalmers University of Technology, GÃ¶teborg, Sweden</affiliation>
		<affiliation numeration="3" content_type="html">UniversitÃ© Bordeaux 1, CNRS/INSU, Laboratoire d&apos;Astrophysique de Bordeaux, Floirac, France</affiliation>
		<affiliation numeration="4" content_type="html">Laboratoire d&apos;AÃ©rologie, Toulouse, France</affiliation>
		<affiliation numeration="5" content_type="html">University of Saskatchewan, Saskatoon, Canada</affiliation>
		<affiliation numeration="6" content_type="html">York University, Toronto, Canada</affiliation>
		<affiliation numeration="7" content_type="html">Computational Physics, Inc., Boulder, Colorado, USA</affiliation>
		<affiliation numeration="8" content_type="html">Laboratory for Atmospheric and Space Physics, Univ. of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="9" content_type="html">Naval Research Laboratory, Washington, D.C., USA</affiliation>
		<affiliation numeration="10" content_type="html">Laboratoire de Physique et de Chimie de l&apos;Environnement, OrlÃ©ans, France</affiliation>
		<affiliation numeration="11" content_type="html">Department of Physics, University of Toronto, Toronto, Canada</affiliation>
		<affiliation numeration="12" content_type="html">Environment Canada, Toronto, Canada</affiliation>
		<affiliation numeration="13" content_type="html">Service dâ€™AÃ©ronomie, Paris, France</affiliation>
		<affiliation numeration="14" content_type="html">La Trobe University, Victoria, Australia</affiliation>
	</affiliations>
	<abstract content_type="html">The Odin satellite carries two instruments capable of determining
stratospheric ozone profiles by limb sounding: the Sub-Millimetre Radiometer
(SMR) and the UV-visible spectrograph of the OSIRIS (Optical Spectrograph and
InfraRed Imager System) instrument. A large number of ozone profiles
measurements were performed during six years from November 2001 to present.
This ozone dataset is here used to make quantitative comparisons with
satellite measurements in order to assess the quality of the Odin/SMR ozone
measurements. In a first step, we compare Swedish SMR retrievals version 2.1,
French SMR ozone retrievals version 222 (both from the 501.8 GHz band), and
the OSIRIS retrievals version 3.0, with the operational version 4.0 ozone
product from POAM III (Polar Ozone Atmospheric Measurement). In a second
step, we refine the Odin/SMR validation by comparisons with ground-based
instruments and balloon-borne observations. We use observations carried out
within the framework of the Network for Detection of Atmospheric Composition
Change (NDACC) and balloon flight missions conducted by the Canadian Space
Agency (CSA), the Laboratoire de Physique et de Chimie de l&apos;Environnement
(LPCE, OrlÃ©ans, France), and the Service d&apos;AÃ©ronomie (SA, Paris, France).
Coincidence criteria were 5&amp;deg; in latitude x in 10&amp;deg; longitude, and
5 h in time in Odin/POAM III comparisons, 12 h in Odin/NDACC
comparisons, and 72 h in Odin/balloons comparisons. An agreement is found
with the POAM III experiment (10&amp;ndash;60 km) within &amp;minus;0.3&amp;plusmn;0.2 ppmv
(bias&amp;plusmn;standard deviation) for SMR (v222, v2.1) and within &amp;minus;0.5&amp;plusmn;0.2 ppmv
for OSIRIS (v3.0). Odin ozone mixing ratio products are systematically
slightly lower than the POAM III data and show an ozone maximum lower by 1&amp;ndash;5 km
in altitude. The comparisons with the NDACC data (10&amp;ndash;34 km for ozonesonde,
10&amp;ndash;50 km for lidar, 10&amp;ndash;60 for microwave instruments) yield a good agreement
within &amp;minus;0.15&amp;plusmn;0.3 ppmv for the SMR data and &amp;minus;0.3&amp;plusmn;0.3 ppmv for the
OSIRIS data. Finally the comparisons with instruments on large balloons
(10&amp;ndash;31 km) show a good agreement, within &amp;minus;0.7&amp;plusmn;1 ppmv.</abstract>
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</article>

