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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-13-1455-2013</article-id>
<title-group>
<article-title>New particle formation in the western Yangtze River Delta: first data from SORPES-station</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Herrmann</surname>
<given-names>E.</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>Ding</surname>
<given-names>A. J.</given-names>
<ext-link>https://orcid.org/0000-0003-4481-5386</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Petäjä</surname>
<given-names>T.</given-names>
<ext-link>https://orcid.org/0000-0002-1881-9044</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yang</surname>
<given-names>X. Q.</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>Sun</surname>
<given-names>J. 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>Qi</surname>
<given-names>X. 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>Manninen</surname>
<given-names>H.</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>Hakala</surname>
<given-names>J.</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>Nieminen</surname>
<given-names>T.</given-names>
<ext-link>https://orcid.org/0000-0002-2713-715X</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Aalto</surname>
<given-names>P. P.</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>Kerminen</surname>
<given-names>V.-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>Kulmala</surname>
<given-names>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>Fu</surname>
<given-names>C. B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Atmospheric Sciences and Institute for Climate and Global Change Research, Nanjing University, Nanjing,  China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Physics, University of Helsinki, Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>01</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>1</issue>
<fpage>1455</fpage>
<lpage>1488</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 E. Herrmann et al.</copyright-statement>
<copyright-year>2013</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/preprints/13/1455/2013/acpd-13-1455-2013.html">This article is available from https://acp.copernicus.org/preprints/13/1455/2013/acpd-13-1455-2013.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/13/1455/2013/acpd-13-1455-2013.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/13/1455/2013/acpd-13-1455-2013.pdf</self-uri>
<abstract>
<p>Aerosols and new particle formation were studied in the western part
      of the Yangtze River Delta (YRD), at the SORPES station of Nanjing
      University. Air ions between 0.8 and 42 nm were measured using
      an air ion spectrometer; a DMPS provided particle size distributions
      between 6 and 800 nm. Additionally, meteorological data, trace
      gas concentrations, and PM&lt;sub&gt;2.5&lt;/sub&gt; values were recorded. During
      the measurement period from 18 November 2011 to 31 March 2012, the
      mean total particle concentration was found to be
      23 000 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. The mean PM&lt;sub&gt;2.5&lt;/sub&gt; value was
      90 &amp;mu; g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, well above national limits. During the
      observations, 26 new particle formation events occurred, typically
      producing 6 nm particles at a rate of
      1 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, resulting in over 4000 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; new
      CCN per event. Typical growth rates were between 6 and
      7 nm h&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. Ion measurements showed the typical cluster band
      below 2 nm, with total ion concentrations roughly between 600
      and 1000 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. A peculiar feature of the ion measurements
      were the heightened ion cluster concentrations during the nights
      before event days. The highly polluted air of the YRD provides both
      the potential source (SO&lt;sub&gt;2&lt;/sub&gt;) and the sink (particulate matter)
      for sulfuric acid, leaving radiation as the determining force behind
      new particle formation. Accordingly, a good correlation was found
      between new particle formation rate and radiation values.</p>
</abstract>
<counts><page-count count="34"/></counts>
</article-meta>
</front>
<body/>
<back>
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