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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-7-9973-2007</article-id>
<title-group>
<article-title>MIPAS reference atmospheres and comparisons to V4.61/V4.62 MIPAS level 2 geophysical  data sets</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Remedios</surname>
<given-names>J. J.</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>Leigh</surname>
<given-names>R. J.</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>Waterfall</surname>
<given-names>A. M.</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>Moore</surname>
<given-names>D. 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>Sembhi</surname>
<given-names>H.</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>Parkes</surname>
<given-names>I.</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>Greenhough</surname>
<given-names>J.</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>Chipperfield</surname>
<given-names>M.P.</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>Hauglustaine</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>EOS, Space Research Centre, Department of Physics and Astronomy, University of Leicester, Leicester, LE1 7RH, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Atmospheric Science, Space Science and Technology Department, CCLRC Rutherford  Appleton Laboratory, Chilton, Didcot, Oxfordshire, OX11 0QX, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of the Environment, University of Leeds, Leeds, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>LSCE, CNRS/CEA, l&apos;Orme-des-Merisiers, 91191 Gif-sur-Yvette, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>07</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>4</issue>
<fpage>9973</fpage>
<lpage>10017</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<abstract>
<p>Reliable reference profiles and estimates of variability are a
necessity for a variety of processes relating to ENVISAT including
the development of key aspects and inputs for the operational
processor for the Michelson Interferometer for Passive Atmospheric
Sounding. MIPAS reference atmospheres have therefore been produced
in two forms, namely standard atmospheres for modelling and error
analysis for typical atmospheric situations and the IG2 seasonal
climatologies for initial guess profiles used as part of the
operational processing. The reference states cover 36 species on a
common altitude, pressure, and temperature grid from 0 to 120 km,
and include both means and estimates of variability (maximum,
minimum and one sigma values). This paper describes V3.1 of the standard
atmospheres and V4.0 of the IG2 atmospheres which are the current
versions of the reference atmospheres. Particular attention is paid
to the MIPAS operational geophysical products (pressure/temperature,
H&lt;sub&gt;2&lt;/sub&gt;O, O&lt;sub&gt;3&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O, HNO&lt;sub&gt;3&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt;) and to CO&lt;sub&gt;2&lt;/sub&gt;
whose mixing ratio is required for the retrieval of pressure and
temperature. A dynamic representation of CO&lt;sub&gt;2&lt;/sub&gt; is presented which
shows the presence of CO&lt;sub&gt;2&lt;/sub&gt; gradients in the troposphere and the
lower stratosphere.
&lt;br&gt;&lt;br&gt;
Since these atmospheres have been produced independently of MIPAS
data, it is also possible to compare the data to the MIPAS
operational products and derive valuable information on both the
reference atmospheres and on MIPAS data products themselves. This
process has been performed for V4.61/V4.62 data from the year 2003
as part of the MIPAS validation activity. It is demonstrated that
the agreement between the MIPAS mean data and the reference
atmospheres is very good in mid-latitudes and the tropics, verifying
these data to first order. There is also reasonable agreement in
standard deviations between the IG2 atmospheres and the
corresponding sigmas calculated from the MIPAS data. Knowledge of
tropospheric concentrations of CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O is used to examine
the accuracy of the MIPAS data and their susceptibility to cloud
effects. It is shown that for the highest accuracy, MIPAS data
should be filtered with cloud index values of 2.5 for N&lt;sub&gt;2&lt;/sub&gt;O and 3.5
for CH&lt;sub&gt;4&lt;/sub&gt;. Once such filtering has been performed, the MIPAS data
for these species appear to be accurate to within 10% in the upper
troposphere. The use of cloud index data in combination with MIPAS
data is recommended for studies of the polar winter stratosphere and
the upper troposphere/lower stratosphere.</p>
</abstract>
<counts><page-count count="45"/></counts>
</article-meta>
</front>
<body/>
<back>
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