<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>2</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/acpd-2-1791-2002</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/2/1791/2002/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/2/1791/2002/acpd-2-1791-2002.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/2/1791/2002/acpd-2-1791-2002.pdf</fulltext_pdf>
	<start_page>1791</start_page>
	<end_page>1807</end_page>
	<publication_date>2002-10-28</publication_date>
	<article_title content_type="html">A model for particle formation and growth in the atmosphere with molecular resolution in size</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. E. J. Lehtinen</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Kulmala</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Helsinki University, Dept. Physical Sciences, P.O. Box 64, 00014 Univ. of Helsinki, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">The formation and growth of atmospheric aerosol particles is considered using an exact
      discrete method with molecular resolution in size space. The method is immune to numerical
      diffusion problems that are a nuisance for typical simulation methods using a sectional
      representation for the particle size distribution. For condensational growth, a slight
      modification is proposed for the Fuchs-Sutugin expression, which improves the prediction of
      the growth rate of nano-sized particles by as much as a factor of two. The presented method is
      applied to particle formation in a Finnish Boreal forest and is shown to capture the essential
      features of the dynamics quite nicely. Furthermore, it is shown that the growth of the particles
      is roughly linear, which means that the amount of condensable vapour is constant (of the
      order 10&lt;sup&gt;13&lt;/sup&gt; 1/m&lt;sup&gt;3&lt;/sup&gt;).</abstract>
	<references>
	</references>
</article>

