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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-3-5139-2003</article-id>
<title-group>
<article-title>Urban aerosol number size distributions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hussein</surname>
<given-names>T.</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>Puustinen</surname>
<given-names>A.</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>Aalto</surname>
<given-names>P. 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>Mäkelä</surname>
<given-names>J. 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>Hämeri</surname>
<given-names>K.</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>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physical Sciences, University of Helsinki, P.O. Box 64, FIN-00014, UHEL, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Physics, Tampere University of Technology, P.O. Box 692, FIN-33101 Tampere, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Physics Department, Finnish Institute of Occupational Health, Topeliuksenkatu 41a A, FIN-00250 Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>10</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>5</issue>
<fpage>5139</fpage>
<lpage>5184</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/3/5139/2003/acpd-3-5139-2003.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/3/5139/2003/acpd-3-5139-2003.pdf</self-uri>
<abstract>
<p>Aerosol number size distributions were measured continuously in Helsinki,
      Finland from 5 May 1997 to 28 February 2003. The daily, monthly and annual
      patterns were investigated. The temporal variation of the particle number concentration was seen to follow the traffic density. The highest total
      particle number concentrations were usually observed during workdays; especially on Fridays, and the lower concentrations occurred during weekends;
      especially Sundays. Seasonally, the highest total number concentrations were
      usually observed during winter and spring and the lowest during June and July. More than 80\% of the particle number size distributions were
      tri-modal: nucleation mode (Dp &amp;lt; 30 nm), Aitken mode (20&amp;ndash;100 nm) and accumulation mode
      (Dp &amp;gt; 90 nm). Less than 20% of the particle number size distributions have either two modes or consisted of more than three modes.
      Two different measurement sites are used; in the first place (Siltavuori, 5
      May 1997&amp;ndash;5 March 2001), the overall means of the integrated particle number
      concentrations were 7100 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, 6320 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, and 960 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;,
      respectively, for nucleation, Aitken, and accumulation modes. In the second
      site (Kumpula, 6 March 2001&amp;ndash;28 February 2003) they were 5670 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;,
      4050 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, and 900 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. The total number concentration in
      nucleation and Aitken modes were usually significantly higher during weekdays
      than during weekends. The variations in accumulation mode were less pronounced. The smaller concentrations in Kumpula were mainly due to building
      construction and also slight overall decreasing trend during these years. During the site changing a period of simultaneous measurements over two weeks
      were performed showing nice correlation in both sites.</p>
</abstract>
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