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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-3-1477-2003</article-id>
<title-group>
<article-title>Fine and ultrafine particles in the Zürich (Switzerland) area measured with a mobile laboratory: an assessment of the seasonal and regional variation throughout a year</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bukowiecki</surname>
<given-names>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>Dommen</surname>
<given-names>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>Prévôt</surname>
<given-names>A. S. H.</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>Weingartner</surname>
<given-names>E.</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>Baltensperger</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratory of Atmospheric Chemistry, Paul Scherrer Institut, CH-5232 Villigen PSI, Switzerland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>24</day>
<month>09</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>5</issue>
<fpage>1477</fpage>
<lpage>1494</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/3/1477/2003/acp-3-1477-2003.html">This article is available from http://www.atmos-chem-phys.net/3/1477/2003/acp-3-1477-2003.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/3/1477/2003/acp-3-1477-2003.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/3/1477/2003/acp-3-1477-2003.pdf</self-uri>
<abstract>
<p>On occasion of the project YOGAM (year of gas phase and aerosol
      measurements), the spatial and temporal variation of selected aerosol and gas phase parameters was assessed for the
      Zürich (Switzerland) area with a new mobile pollutant measurement laboratory. This assessment based on on-road measurements along a
      specified route on selected days during different seasons in 2001/2002, covering urban, suburban and rural regions. Special
      focus was put on the investigation and characterization of particles in the fine (particle diameter
      D&amp;lt;2.5 &lt;font face=&quot;Symbol&quot;&gt;m&lt;/font&gt;m) and
      ultrafine (D&amp;lt;100 nm) size ranges. Analysis of Variance (ANOVA) showed that the variance of all considered fine and ultrafine
      aerosol parameters (i.e. particle background and total number concentration for particles larger than
      3 nm, number concentrations in the size ranges 7-30 nm and 80-140 nm, as well as the active surface area concentration) was significantly
      larger for day-to-day than for spatial variation. However, Principal Component Analysis
      (PCA) found a similar regional pollution pattern within every single measuring day. Lowest
      particle background levels (D&amp;gt;3 nm) were found in rural areas at higher elevation
      (15 000 cm&lt;sup&gt;-3&lt;/sup&gt;), while corresponding mean background values for urban and freeway-influenced areas were
      typically 35 000 cm&lt;sup&gt;-3&lt;/sup&gt; and &amp;gt;80 000 cm&lt;sup&gt;-3&lt;/sup&gt;, respectively. Meteorology, i.e. prevailing weather conditions not
      only governed the day-to-day concentration variations in the selected area, but also influenced the formation of primary
      (directly traffic-related) and in few cases secondary (biogenic or anthropogenic) ultrafine particles. Overall, low temperatures
      regularly enhanced primary ultrafine particle formation in urban areas. There was a possible indication for relatively low number
      concentrations of secondary ultrafine particles during a few warm and sunny spring days. Mobile measurements as they were performed
      in this study have been shown to be suitable for pollutant assessments to obtain good information on spatial and day-to-day
      variability. For experimental studies concerning spatial resolution on a relatively short time scale
      (&amp;lt;1 day), a mobile measurement design may even be more appropriate than a network of
      stationary measuring sites.</p>
</abstract>
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