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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-12-3261-2012</article-id>
<title-group>
<article-title>CO at 40–80 km above Kiruna observed by the ground-based microwave radiometer KIMRA and simulated by the Whole Atmosphere Community Climate Model</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hoffmann</surname>
<given-names>C. G.</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>Kinnison</surname>
<given-names>D. E.</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>Garcia</surname>
<given-names>R. R.</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>Palm</surname>
<given-names>M.</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>Notholt</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>Raffalski</surname>
<given-names>U.</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>Hochschild</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics, University Bremen, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>National Center for Atmospheric Research, Boulder, Colorado, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Swedish Institute of Space Physics, Kiruna, Sweden</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>7</issue>
<fpage>3261</fpage>
<lpage>3271</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 C. G. Hoffmann et al.</copyright-statement>
<copyright-year>2012</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/12/3261/2012/acp-12-3261-2012.html">This article is available from https://acp.copernicus.org/articles/12/3261/2012/acp-12-3261-2012.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/12/3261/2012/acp-12-3261-2012.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/12/3261/2012/acp-12-3261-2012.pdf</self-uri>
<abstract>
<p>This study compares CO in the Arctic stratosphere and mesosphere measured by ground-based
  microwave radiometry with simulations made with the Whole Atmosphere Community Climate Model
  driven with specified dynamical fields (SD-WACCM4) for the Arctic winters 2008/2009 and
  2009/2010. CO is a tracer for polar winter middle atmosphere dynamics, hence the
  representation of polar dynamics in the model is examined indirectly. Measurements were taken with
  the KIruna Microwave RAdiometer (KIMRA). The instrument, which is located in Kiruna, Northern
  Sweden (67.8&amp;deg; N, 20.4&amp;deg; E), provides CO profiles between 40 and
  80 km altitude.
&lt;br&gt;&lt;br&gt;
  The present comparison, which is one of the first between SD-WACCM4 and measurements, is performed
  on the smallest space and time scales currently simulated by the model; the global model is
  evaluated daily at the particular model grid-point closest to Kiruna. As a guide to what can
  generally be expected from such a comparison, the same analysis is repeated for observations of
  CO from the Microwave Limb Sounder (MLS), a microwave radiometer onboard NASA&apos;s Aura
  satellite, which has global coverage. First, time-mean profiles of CO are compared, revealing that
  the profile shape of KIMRA deviates from SD-WACCM4 and MLS, especially in the upper
  mesosphere. SD-WACCM4 and MLS are mostly consistent throughout the range  of altitude considered;
  however, SD-WACCM4 shows slightly lower values in the upper mesosphere. 
  Second, the time evolution is compared for the complete time series, as well as for the
  slowly and rapidly evolving parts alone. Overall, the agreement among the datasets is very good
  and the model is almost as consistent with the measurements as the measurements are with each
  other. Mutual correlation coefficients of the slowly varying part of the CO time series are
  ≥0.9 over a wide altitude range. This demonstrates that the polar winter middle atmosphere
  dynamics is very well represented in SD-WACCM4 and that the relaxation to analyzed meteorological
  fields below 50 km constrains the behavior of the simulation sufficiently, even at higher
  altitudes, such that the simulation above 50 km is close to the measurements. However, above
  50 km, the model-measurement correlation for the rapidly varying part of the CO time
  series is lower (0.3) than the measurement-measurement correlation (0.6). This is attributed to
  the fact that the gravity wave parametrization in WACCM is based on a generic gravity wave
  spectrum and cannot be expected to capture the instantaneous behavior of the actual gravity wave
  field present in the atmosphere.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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