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<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-6-5549-2006</article-id>
<title-group>
<article-title>Using discriminant analysis as a nucleation event classification method</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mikkonen</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>Lehtinen</surname>
<given-names>K. E. J.</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>Hamed</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>Joutsensaari</surname>
<given-names>J.</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>Facchini</surname>
<given-names>M. C.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Laaksonen</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>Department of Physics, University of Kuopio, P.O. Box 1627, 70211 Kuopio, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Finnish meteorological institute, Kuopio Unit, P.O. Box 1627, 70210 Kuopio, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Environmental Sciences, University of Kuopio, P.O. Box 1627, 70211 Kuopio, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Istituto di Scienze dell&apos;Atmosfera e del Clima &amp;ndash; CNR, Italy Via Gobetti 101, 40 129 Bologna, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>12</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>12</issue>
<fpage>5549</fpage>
<lpage>5557</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/6/5549/2006/acp-6-5549-2006.html">This article is available from http://www.atmos-chem-phys.net/6/5549/2006/acp-6-5549-2006.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/6/5549/2006/acp-6-5549-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/6/5549/2006/acp-6-5549-2006.pdf</self-uri>
<abstract>
<p>More than three years of measurements of aerosol size-distribution and
different gas and meteorological parameters made in Po Valley, Italy were
analysed for this study to examine which of the meteorological and trace gas
variables effect on the emergence of nucleation events. As the analysis
method, we used discriminant analysis with non-parametric Epanechnikov
kernel, included in non-parametric density estimation method. The best
classification result in our data was reached with the combination of
relative humidity, ozone concentration and a third degree polynomial of
radiation. RH appeared to have a preventing effect on the new particle
formation whereas the effects of O&lt;sub&gt;3&lt;/sub&gt; and radiation were more conductive.
The concentration of SO&lt;sub&gt;2&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt; also appeared to have significant
effect on the emergence of nucleation events but because of the great amount
of missing observations, we had to exclude them from the final analysis.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</article>