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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-8-18155-2008</article-id>
<title-group>
<article-title>Spatio-temporal variability and principal components of the particle number size distribution  in an urban atmosphere</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Costabile</surname>
<given-names>F.</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>Birmili</surname>
<given-names>W.</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>Klose</surname>
<given-names>S.</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>Tuch</surname>
<given-names>T.</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>Wehner</surname>
<given-names>B.</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>Wiedensohler</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>Franck</surname>
<given-names>U.</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>KÃ¶nig</surname>
<given-names>K.</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>Sonntag</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Leibniz Institute for Tropospheric Research, Leipzig, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>C.N.R. â€“ IIA, Via Salaria Km 29, 3, 00016 Monterotondo Scalo (Roma), Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Helmholtz Center for Environmental Research, Leipzig, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>10</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>5</issue>
<fpage>18155</fpage>
<lpage>18217</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/8/18155/2008/acpd-8-18155-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/8/18155/2008/acpd-8-18155-2008.pdf</self-uri>
<abstract>
<p>Due to the presence of diffusive anthropogenic sources in urban areas, the spatio-temporal
variability of fine (diameter &amp;lt;1 Î¼m) and ultrafine (&amp;lt;0.1 Î¼m) aerosol particles
has been a challenging issue in particle exposure assessment as well as atmospheric research in
general. We examined number size distributions of atmospheric aerosol particles (size range
3â€“800 nm) that were measured simultaneously at a maximum of eight observation sites in and around
a city in Central Europe (Leipzig, Germany). Two main experiments were conducted with different
time span and number of observation sites (2 years at 3 sites; 1 month at 8 sites). A general
observation was that the particle number size distribution varied in time and space in a complex
fashion as a result of interaction between local and far-range sources, and the meteorological
conditions. To identify statistically independent factors in the urban aerosol, different runs of
principal component analysis were conducted encompassing aerosol, gas phase, and meteorological
parameters from the multiple sites. Several of the resulting principal components, outstanding with
respect to their temporal persistence and spatial coverage, could be associated with aerosol
particle modes: a first accumulation mode (&quot;droplet mode&quot;, 300â€“800 nm), considered to be the
result of liquid phase processes and far-range transport; a second accumulation mode (centered
around diameters 90â€“250 nm), considered to result from primary emissions as well as aging through
condensation and coagulation; an Aitken mode (30â€“200 nm) linked to urban traffic emissions in
addition to an urban and a rural Aitken mode; a nucleation mode (5â€“20 nm) linked to urban traffic
emissions; nucleation modes (3â€“20 nm) linked to photochemically induced particle formation; an
aged nucleation mode (10â€“50 nm). A number of additional components were identified to represent
only local sources at a single site each, or infrequent phenomena. In summary, the analysis of size
distributions of high time and size resolution yielded a surprising wealth of statistical aerosol
components occurring in the urban atmosphere over one single city. Meanwhile, satisfactory physical
explanations could be found for the components with the greatest temporal persistence and spatial
coverage. Therefore a paradigm on the behaviour of sub-Î¼m urban aerosol particles is proposed,
with recommendations how to efficiently monitor individual sub-fractions across an entire city.</p>
</abstract>
<counts><page-count count="63"/></counts>
</article-meta>
</front>
<body/>
<back>
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