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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-9-23141-2009</article-id>
<title-group>
<article-title>Latitudinal gradient and interannual variation of PM&lt;sub&gt;10&lt;/sub&gt; concentration over eighty-six Chinese cities</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Qu</surname>
<given-names>W. 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>Arimoto</surname>
<given-names>R.</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>Zhang</surname>
<given-names>X. Y.</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>Wang</surname>
<given-names>Y. Q.</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>Sheng</surname>
<given-names>L. F.</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>Fu</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Key Laboratory of Physical Oceanography, Ocean-Atmosphere  Interaction and Climate Laboratory, Department of Marine Meteorology, College of Physical  and Environmental Oceanography, Ocean University of China, 238 Songling Rd., Qingdao 266100, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Key Laboratory of Atmospheric Chemistry, Centre for Atmosphere Watch and Services (CAWAS),  Chinese Academy of Metrological Sciences, China Meteorological Administration, 46 Zhong-Guan-Cun S. Ave., Beijing 100081, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Carlsbad Environmental Monitoring and Research Center, New Mexico State University, Carlsbad, New Mexico, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>11</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>6</issue>
<fpage>23141</fpage>
<lpage>23185</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/9/23141/2009/acpd-9-23141-2009.html">This article is available from http://www.atmos-chem-phys-discuss.net/9/23141/2009/acpd-9-23141-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/23141/2009/acpd-9-23141-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/23141/2009/acpd-9-23141-2009.pdf</self-uri>
<abstract>
<p>The spatial distribution of the aerosols over 86 major Chinese cities was constructed from
      137 845 daily averaged PM&lt;sub&gt;10&lt;/sub&gt; (particles with diameter &amp;le;10 &amp;mu;m)
      concentrations calculated from air pollution index (API) records spanning from summer 2000
      to winter 2006. This dataset was based on days when PM&lt;sub&gt;10&lt;/sub&gt; was categorized as the
      principal pollutant, accounting for 91.6% of the total recorded days. The 83 cities in
      mid-eastern China (longitude 100&amp;deg; E to 130&amp;deg; E) were separated into three
      latitudinal zones with the Qinlin Mountain – the Huaihe River and the Yunnan-Guizhou
      Plateau – the Jiangnan Hill – the Wuyi Mountain as the boundaries. The spatial
      distribution of PM&lt;sub&gt;10&lt;/sub&gt; was complicated; the high-value spots in northern China
      (concentration ranged from 127.1 to 192.1 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) included Urumchi,
      Lanzhou-Xining, Weinan-Xi&apos;an, Taiyuan-Datong-Yangquan-Changzhi, Pingdingshan-Kaifeng,
      Beijing-Tianjin-Shijiazhuang, Jinan, and Shenyang-Anshan-Fushun; in the middle zone, the
      high PM&lt;sub&gt;10&lt;/sub&gt; spots (concentration within 119.1–146.6 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) were
      Chongqing-Chengdu-Luzhou, Changsha-Wuhan, and Nanjing-Hangzhou; while in the southern zone,
      four cities (Qujing, Guiyang, Guangzhou and Shaoguan) showed higher PM&lt;sub&gt;10&lt;/sub&gt;
      concentration (&amp;gt;80 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;). An overall latitudinal gradient was distinct;
      the median PM&lt;sub&gt;10&lt;/sub&gt; concentrations decreased from 108 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for the
      38 northern cities to 95 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; and 55 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for the middle
      (26 cities) and southern (19 cities) zones, respectively. Linear regression between
      PM&lt;sub&gt;10&lt;/sub&gt; concentration and latitude of the cities also confirmed this
      gradient. PM&lt;sub&gt;10&lt;/sub&gt; concentration and the APIs exhibited similar seasonality with
      wintertime maxima and summertime minima, and the second highest values in
      spring. PM&lt;sub&gt;10&lt;/sub&gt; level showed a decreasing trend (&amp;minus;23.2 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;)
      for the northern cities during 2000 to 2006. For the other two zones, the PM&lt;sub&gt;10&lt;/sub&gt;
      levels fluctuated, but showed unobvious change (&amp;minus;1.7 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) for the
      middle zone and increased slightly (+6.2 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) for the southern zone
      during the course.</p>
</abstract>
<counts><page-count count="45"/></counts>
</article-meta>
</front>
<body/>
<back>
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