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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-10-3229-2010</article-id>
<title-group>
<article-title>Ozone predictabilities due to meteorological uncertainties in Mexico City basin using ensemble forecasts</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bei</surname>
<given-names>N.</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>Lei</surname>
<given-names>W.</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>Zavala</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>Molina</surname>
<given-names>L. T.</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-group><aff id="aff1">
<label>1</label>
<addr-line>Molina Center for Energy and the Environment, La Jolla, CA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Earth, Atmospheric and Planetary Sciences, Massachusetts  Institute of Technology, Cambridge, MA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>02</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>2</issue>
<fpage>3229</fpage>
<lpage>3263</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-discuss.net/10/3229/2010/acpd-10-3229-2010.html">This article is available from http://www.atmos-chem-phys-discuss.net/10/3229/2010/acpd-10-3229-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/10/3229/2010/acpd-10-3229-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/10/3229/2010/acpd-10-3229-2010.pdf</self-uri>
<abstract>
<p>The purpose of the present study is to investigate the sensitivity of
      ozone concentration ([O&lt;sub&gt;3&lt;/sub&gt;]) predictions in Mexico City to
      meteorological initial uncertainties and planetary boundary layer
      (PBL) parameterization schemes using state-of-the-art meteorological
      and photochemical prediction models through ensemble forecasts. The
      simulated periods (3, 9, 15, and 29 March 2006), represent four typical
      meteorological episodes (&amp;quot;South-Venting&amp;quot;,
&amp;quot;O&lt;sub&gt;3&lt;/sub&gt;-North&amp;quot;, &amp;quot;O&lt;sub&gt;3&lt;/sub&gt;-South&amp;quot; and
&amp;quot;Convection-North&amp;quot;, respectively) in the Mexico City basin during
      the MCMA-2006/MILAGRO campaign. Our results demonstrate that
      uncertainties in meteorological initial conditions have significant
      impacts on O&lt;sub&gt;3&lt;/sub&gt; predictions, including the peak time
      [O&lt;sub&gt;3&lt;/sub&gt;], as well as the horizontal and vertical [O&lt;sub&gt;3&lt;/sub&gt;]
      distributions, and temporal variations. The ensemble spread of the
      simulated peak [O&lt;sub&gt;3&lt;/sub&gt;] averaged over the city&apos;s ambient
      monitoring sites can reach up to 10 ppb. The magnitude of the
      ensemble spreads varies with different PBL schemes and meteorological
      episodes. The uncertainties in O&lt;sub&gt;3&lt;/sub&gt; predictions caused by PBL
      schemes mainly come from their ability to represent the mixing layer
      height, but overall, these uncertainties are smaller than those from
      uncertainties in meteorological initial conditions.</p>
</abstract>
<counts><page-count count="35"/></counts>
</article-meta>
</front>
<body/>
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