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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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>
</journal-title-group>
<issn pub-type="epub">1680-7324</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/acp-4-391-2004</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>01</day>
<month>03</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>2</issue>
<fpage>391</fpage>
<lpage>411</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.net/4/391/2004/acp-4-391-2004.html">This article is available from http://www.atmos-chem-phys.net/4/391/2004/acp-4-391-2004.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/4/391/2004/acp-4-391-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/391/2004/acp-4-391-2004.pdf</self-uri>
<abstract>
<p>Aerosol number size distributions have been measured since 5 May 1997 in
Helsinki, Finland. The presented aerosol data represents size distributions
within the particle diameter size range 8-400nm during the period from
May 1997 to March 2003. The daily, monthly and annual patterns of the
aerosol particle number concentrations were investigated. The temporal
variation of the particle number concentration showed close correlations
with traffic activities. The highest total number concentrations were
observed during workdays; especially on Fridays, and the lowest
concentrations occurred during weekends; especially Sundays. Seasonally, the
highest total number concentrations were observed during winter and spring
and lower concentrations were observed during June and July. More than
80% of the number size distributions had three modes: nucleation mode
(&lt;IMG WIDTH=&quot;36&quot; HEIGHT=&quot;30&quot; ALIGN=&quot;MIDDLE&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img1.gif&quot;  
 ALT=&quot;$D_{p}{&amp;lt;}$&quot;&gt;30nm), Aitken mode (20-100nm) and accumulation mode
(&lt;IMG WIDTH=&quot;36&quot; HEIGHT=&quot;30&quot; ALIGN=&quot;MIDDLE&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img2.gif&quot;  
 ALT=&quot;$D_{p}{&amp;gt;}$&quot;&gt;90nm). Less than 20% of the number size distributions had
either two modes or consisted of more than three modes. Two different
measurement sites were used; in the first (Siltavuori, 5.5.1997-5.3.2001),
the arithmetic means of the particle number concentrations were 7000cm&lt;IMG WIDTH=&quot;20&quot; HEIGHT=&quot;18&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img3.gif&quot;  
 ALT=&quot;$^{-3}$&quot;&gt;,
6500cm&lt;IMG WIDTH=&quot;20&quot; HEIGHT=&quot;18&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img3.gif&quot;  
 ALT=&quot;$^{-3}$&quot;&gt;, and 1000cm&lt;IMG WIDTH=&quot;20&quot; HEIGHT=&quot;18&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img3.gif&quot;  
 ALT=&quot;$^{-3}$&quot;&gt; respectively for nucleation,
Aitken, and accumulation modes. In the second site (Kumpula,
6.3.2001-28.2.2003) they were 5500cm&lt;IMG WIDTH=&quot;20&quot; HEIGHT=&quot;18&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img3.gif&quot;  
 ALT=&quot;$^{-3}$&quot;&gt;, 4000cm&lt;IMG WIDTH=&quot;20&quot; HEIGHT=&quot;18&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img3.gif&quot;  
 ALT=&quot;$^{-3}$&quot;&gt;, and 1000cm&lt;IMG WIDTH=&quot;20&quot; HEIGHT=&quot;18&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-391-img3.gif&quot;  
 ALT=&quot;$^{-3}$&quot;&gt;.
The total number concentration in nucleation and Aitken modes
were usually significantly higher during workdays than during weekends. The
temporal variations in the accumulation mode were less pronounced. The lower
concentrations at Kumpula were mainly due to building construction and also
the slight overall decreasing trend during these years. During the site
changing a period of simultaneous measurements over two weeks were performed
showing nice correlation at both sites.</p>
</abstract>
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