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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>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-5-451-2005</article-id>
<title-group>
<article-title>A practical demonstration on AMSU retrieval precision for upper tropospheric humidity by a non-linear multi-channel regression method</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jiménez</surname>
<given-names>C.</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>Eriksson</surname>
<given-names>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>John</surname>
<given-names>V. O.</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>Buehler</surname>
<given-names>S. A.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of GeoSciences, The University of Edinburgh, Edinburgh, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Radio and Space Science, Chalmers University of Technology, Gothenburg, Sweden</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Environmental Physics, University of Bremen, Bremen, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>02</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>2</issue>
<fpage>451</fpage>
<lpage>459</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>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/451/2005/acp-5-451-2005.html">This article is available from http://www.atmos-chem-phys.net/5/451/2005/acp-5-451-2005.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/451/2005/acp-5-451-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/5/451/2005/acp-5-451-2005.pdf</self-uri>
<abstract>
<p>A neural network algorithm inverting selected channels from the
  Advance Microwave Sounding Unit instruments AMSU-A and AMSU-B was
  applied to retrieve layer averaged relative humidity. The neural
  network was trained with a global synthetic dataset representing
  clear-sky conditions. A precision of around 6% was obtained when
  retrieving global simulated radiances, the precision deteriorated
  less than 1% when real mid-latitude AMSU radiances were inverted
  and compared with co-located data from a radiosonde station. The 6%
  precision outperforms by 1% the reported precision estimate
  from a linear single-channel regression between radiance and
  weighting function averaged relative humidity, the more traditional
  approach to exploit AMSU data. Added advantages are not only a
  better precision; the AMSU-B humidity information is more optimally
  exploited by including temperature information from AMSU-A channels;
  and the layer averaged humidity is a more physical quantity than the
  weighted humidity, for comparison with other datasets.  The training
  dataset proved adequate for inverting real radiances from a
  mid-latitude site, but it is limited by not considering the impact
  of clouds or surface emissivity changes, and further work is needed
  in this direction for further validation of the precision estimates.</p>
</abstract>
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</article-meta>
</front>
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