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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-14-559-2014</article-id>
<title-group>
<article-title>The transport of atmospheric NO&lt;sub&gt;x&lt;/sub&gt; and HNO&lt;sub&gt;3&lt;/sub&gt; over Cape Town</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Abiodun</surname>
<given-names>B. 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>Ojumu</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>Jenner</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>Ojumu</surname>
<given-names>T. V.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Climate Systems Analysis Group, Department of Environmental and Geographical Science, University of Cape Town, South Africa</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Environmental and Agricultural Sciences, University of South Africa, South Africa</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Chemical Engineering, Cape Peninsula University of Technology, South Africa</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>01</month>
<year>2014</year>
</pub-date>
<volume>14</volume>
<issue>2</issue>
<fpage>559</fpage>
<lpage>575</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 B. J. Abiodun et al.</copyright-statement>
<copyright-year>2014</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/14/559/2014/acp-14-559-2014.html">This article is available from https://acp.copernicus.org/articles/14/559/2014/acp-14-559-2014.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/559/2014/acp-14-559-2014.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/14/559/2014/acp-14-559-2014.pdf</self-uri>
<abstract>
<p>Cape Town, the most popular tourist city in Africa, usually experiences air
pollution with unpleasant odour in winter. Previous studies have associated
the pollution with local emission of pollutants within the city. The present
study examines the transport of atmospheric pollutants (NO&lt;sub&gt;x&lt;/sub&gt; and
HNO&lt;sub&gt;3&lt;/sub&gt;) over South Africa and shows how the transport of pollutants from
the Mpumalanga Highveld, a major South African industrial area, may
contribute to the pollution in Cape Town. The study analysed observation data
(2001–2008) from the Cape Town air-quality network and simulation data
(2001–2004) from a regional climate model (RegCM) over southern Africa. The
simulation accounts for the influence of complex topography, atmospheric
conditions, and atmospheric chemistry on emission and transport of pollutants
over southern Africa. Flux budget analysis was used to examine whether Cape
Town is a source or sink for NO&lt;sub&gt;x&lt;/sub&gt; and HNO&lt;sub&gt;3&lt;/sub&gt; during the extreme
pollution events.
&lt;br&gt;&lt;br&gt;
The results show that extreme pollution events in Cape Town are associated
with the lower level (surface – 850 hPa) transport of NO&lt;sub&gt;x&lt;/sub&gt; from
the Mpumalanga Highveld to Cape Town, and with a tongue of high concentration
of HNO&lt;sub&gt;3&lt;/sub&gt; that extends from the Mpumalanga Highveld to Cape Town along the
south coast of South Africa. The prevailing atmospheric conditions during the
extreme pollution events feature an upper-level (700 hPa) anticyclone over
South Africa and a lower-level col over Cape Town. The anticyclone induces a
strong subsidence motion, which prevents vertical mixing of the pollutants
and caps high concentration of pollutants close to the surface as they are
transported from the Mpumalanga Highveld toward Cape Town. The col
accumulates the pollutants over the city. This study shows that Cape Town can
be a sink for the NO&lt;sub&gt;x&lt;/sub&gt; and HNO&lt;sub&gt;3&lt;/sub&gt; during extreme pollution
events and suggests that the accumulation of pollutants transported from
other areas (e.g. the Mpumalanga Highveld) may contribute to the air
pollution in Cape Town.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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