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<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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-9-897-2009</article-id>
<title-group>
<article-title>Global temperature estimates in the troposphere and stratosphere: a validation study of COSMIC/FORMOSAT-3 measurements</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kishore</surname>
<given-names>P.</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>Namboothiri</surname>
<given-names>S. P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jiang</surname>
<given-names>J. H.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sivakumar</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Igarashi</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Dept. of Physics and Atmospheric Science, Dalhousie University, Halifax, Canada</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>National Institute of Information and Communications Technology, Tokyo, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Jet Propulsion Laboratory, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>National Laser Centre, CSIR, Pretoria, South Africa</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Geography, Geoinformatics and Meteorology, University of Pretoria, South Africa</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>02</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>3</issue>
<fpage>897</fpage>
<lpage>908</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2009 P. Kishore et al.</copyright-statement>
<copyright-year>2009</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/9/897/2009/acp-9-897-2009.html">This article is available from https://acp.copernicus.org/articles/9/897/2009/acp-9-897-2009.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/9/897/2009/acp-9-897-2009.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/9/897/2009/acp-9-897-2009.pdf</self-uri>
<abstract>
<p>This paper mainly focuses on the validation of temperature estimates derived
with the newly launched Constellation Observing System for Meteorology
Ionosphere and Climate (COSMIC)/Formosa Satellite 3 (FORMOSAT-3) system. The
analysis is based on the radio occultation (RO) data samples collected
during the first year observation from April 2006 to April 2007. For the
validation, we have used the operational stratospheric analyses including
the National Centers for Environmental Prediction - Reanalysis (NCEP), the
Japanese 25-year Reanalysis (JRA-25), and the United Kingdom Met Office
(MetO) data sets. Comparisons done in different formats reveal good
agreement between the COSMIC and reanalysis outputs. Spatially, the largest
deviations are noted in the polar latitudes, and height-wise, the tropical
tropopause region noted the maximum differences (2–4 K). We found that
among the three reanalysis data sets the NCEP data sets have the best
resemblance with the COSMIC measurements.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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