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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-12-2289-2012</article-id>
<title-group>
<article-title>A numerical comparison of different methods for determining the particle formation rate</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vuollekoski</surname>
<given-names>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>Sihto</surname>
<given-names>S.-L.</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>Kerminen</surname>
<given-names>V.-M.</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>Kulmala</surname>
<given-names>M.</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>Lehtinen</surname>
<given-names>K. E. J.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physics, University of Helsinki, P.O. Box 48, 00014 Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Finnish Meteorological Institute, 00560 Helsinki, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Applied Environmental Science, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Physics and Mathematics, University of Eastern Finland, 70211 Kuopio, Finland</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Finnish Meteorological Institute, 70211 Kuopio, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>03</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>5</issue>
<fpage>2289</fpage>
<lpage>2295</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 H. Vuollekoski et al.</copyright-statement>
<copyright-year>2012</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/12/2289/2012/acp-12-2289-2012.html">This article is available from https://acp.copernicus.org/articles/12/2289/2012/acp-12-2289-2012.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/12/2289/2012/acp-12-2289-2012.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/12/2289/2012/acp-12-2289-2012.pdf</self-uri>
<abstract>
<p>Different methods of determining formation rates of 3 nm particles are
compared, basing on analysis of simulated data, but the results are valid for
analyses of experimental particle size distribution data as well, at least
within the accuracy of the applied model. The study shows that the method of
determining formation rates indirectly from measured number concentration
data of 3–6 nm particles is generally in good agreement with the
theoretical calculation with a systematic error of 0–20%. While this
accuracy is often enough, a simple modification to the approximative equation
for the formation rate is recommended. A brief study on real atmospheric data
implied that in some cases the accuracy gain may be significant.</p>
</abstract>
<counts><page-count count="7"/></counts>
</article-meta>
</front>
<body/>
<back>
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