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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>3</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acp-3-581-2003</doi>
	<article_url>http://www.atmos-chem-phys.net/3/581/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/3/581/2003/acp-3-581-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/3/581/2003/acp-3-581-2003.pdf</fulltext_pdf>
	<start_page>581</start_page>
	<end_page>589</end_page>
	<publication_date>2003-06-02</publication_date>
	<article_title content_type="html">On the formation of radiation fogs under heavily polluted conditions</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 have studied the effect of gaseous pollutants on fog droplet growth
      in heavily polluted air using a model that describes time-dependent sulfate production in the liquid phase and thermodynamical equilibrium between
      the droplets and the gas phase. Our research indicates that the oxidation of
      SO&lt;sub&gt;2&lt;/sub&gt; to sulfate has a significant effect on fog droplet growth especially when hygroscopic trace gases,
      for example HNO&lt;sub&gt;3&lt;/sub&gt; and NH&lt;sub&gt;3&lt;/sub&gt; are present. The increased sulfate production by dissolution of hygroscopic
      gases results from increased pH (caused by absorption of ammonia) and from the increased size of the fog/smog droplets. Our results
      indicate that unactivated fogs may become optically very thick when the droplet concentrations are on the order of several thousand per
      cubic centimeter of air.</abstract>
	<references>
	</references>
</article>

