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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-11-9607-2011</article-id>
<title-group>
<article-title>Cloud-base vertical velocity statistics: a comparison between an atmospheric mesoscale model and remote sensing observations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tonttila</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>O&apos;Connor</surname>
<given-names>E. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Niemelä</surname>
<given-names>S.</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>Räisänen</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>Järvinen</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki,  Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Meteorology Department, University of Reading, Reading,  UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Division of Atmospheric Sciences, Department of Physics,  University of Helsinki, Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>03</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>3</issue>
<fpage>9607</fpage>
<lpage>9633</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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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/11/9607/2011/acpd-11-9607-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/11/9607/2011/acpd-11-9607-2011.pdf</self-uri>
<abstract>
<p>The statistics of cloud-base vertical velocity simulated by
      the non-hydrostatic mesoscale model AROME are compared with
      Cloudnet remote sensing observations at two locations: the ARM
      SGP site in Central Oklahoma, and the DWD observatory at
      Lindenberg, Germany. The results show that, as expected, AROME
      significantly underestimates the variability of vertical
      velocity at cloud-base compared to observations at their
      nominal resolution; the standard deviation of vertical
      velocity in the model is typically 4–6 times smaller than
      observed, and even more during the winter at
      Lindenberg. Averaging the observations to the horizontal scale
      corresponding to the physical grid spacing of AROME (2.5 km)
      explains 70–80% of the underestimation by the
      model. Further averaging of the observations in the horizontal
      is required to match the model values for the standard
      deviation in vertical velocity. This indicates an effective
      horizontal resolution for the AROME model of at least 4 times
      the physically-defined grid spacing. The results illustrate
      the need for special treatment of sub-grid scale variability
      of vertical velocities in kilometer-scale atmospheric models,
      if processes such as aerosol-cloud interactions are to be
      included in the future.</p>
</abstract>
<counts><page-count count="27"/></counts>
</article-meta>
</front>
<body/>
<back>
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