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<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>7</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-13733-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/13733/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/13733/2007/acpd-7-13733-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/13733/2007/acpd-7-13733-2007.pdf</fulltext_pdf>
	<start_page>13733</start_page>
	<end_page>13771</end_page>
	<publication_date>2007-09-20</publication_date>
	<article_title content_type="html">The validity of the kinetic collection equation revisited</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Alfonso</name>
			<email>lesterson@yahoo.com</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>G. B. Raga</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>D. Baumgardner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Universidad Autónoma de la Ciudad de México, México City, 09790 México</affiliation>
		<affiliation numeration="2" content_type="html">Centro de Ciencias de la Atmósfera, UNAM, México City, 04510 México</affiliation>
	</affiliations>
	<abstract content_type="html">The kinetic collection equation (KCE) describes the evolution of
the average droplet spectrum due to successive events of collision and
coalescence. Fluctuations and non-zero correlations present in the
stochastic coalescence process would imply that the size distributions may
not be correctly modelled by the KCE.
&lt;br&gt;&lt;br&gt;
In this study we expand the known analytical studies of the coalescence
equation with some numerical tools such as Monte Carlo simulations of the
coalescence process. The validity time of the KCE was estimated by
calculating the maximum of the ratio of the standard deviation for the
largest droplet mass over all the realizations to the averaged value. A good
correspondence between the analytical and the numerical approaches was found
for all the kernels studied. The expected values from analytical solutions
of the KCE, were compared with true expected values of the stochastic
collection equation (SCE) estimated with Gillespie&apos;s Monte Carlo algorithm
and analytical solutions of the SCE, after and before the breakdown time.
&lt;br&gt;&lt;br&gt;
The possible implications for cloud physics are discussed, in particular the
possibility of application of these results to kernels modified by
turbulence and electrical processes.</abstract>
	<references>
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</article>

