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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>3</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-3241-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/3241/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/3241/2003/acpd-3-3241-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/3241/2003/acpd-3-3241-2003.pdf</fulltext_pdf>
	<start_page>3241</start_page>
	<end_page>3266</end_page>
	<publication_date>2003-06-26</publication_date>
	<article_title content_type="html">Köhler theory for a polydisperse droplet population in the presence of a soluble trace gas, and an application to stratospheric STS droplet growth</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Kokkola</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Romakkaniemi</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. Laaksonen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Applied Physics, University of Kuopio, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">We consider the equilibrium behavior of a polydisperse aqueous droplet
      population as a function of relative humidity (RH) when a soluble trace gas, such as nitric acid, is present in the system. The droplet
      population  experiences a splitting when the RH is increased sufficiently. This splitting is not related to the traditional
      Köhler activation of cloud droplets, as it may occur at relative humidities below
      100%. Remarkably, the splitting always takes place in  such a way that the largest size class of the
      (discretized) droplet population starts taking up the soluble trace gas efficiently,
      growing steeply as a function of RH, and forcing the smaller droplets to shrink. We consider this behavior in terms of open and closed
      system Köhler curves (open system referring to one in which the trace gas concentration remains constant and closed system to one in
      which the gas concentration decreases as a result of uptake of the trace gas). We show how the open and closed system
      Köhler curves are related, and that the splitting of the population can be explained in
      terms of closed system curves crossing the Köhler maxima of the open system curves. We then go on to consider time-dependent situations,
      and show that due to gas-phase mass transfer limitations, the splitting of the size distributions moves toward smaller sizes as the
      rate of RH increase becomes more rapid. Finally, we consider stratospheric supercooled ternary solution droplet populations, and
      show that the splitting described using the new theory may explain observed bimodal size distributions.</abstract>
	<references>
	</references>
</article>

