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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>4</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-3361-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/3361/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/3361/2003/acpd-3-3361-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/3361/2003/acpd-3-3361-2003.pdf</fulltext_pdf>
	<start_page>3361</start_page>
	<end_page>3372</end_page>
	<publication_date>2003-01-07</publication_date>
	<article_title content_type="html">Comment on evidence for surface-initiated homogenous nucleation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. E. Kay</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>V. Tsemekhman</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>B. Larson</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>M. Baker</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>B. Swanson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth and Space Sciences, University of Washington, Seattle, USA</affiliation>
		<affiliation numeration="2" content_type="html">Applied Physics Laboratory, University of Washington, Seattle, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We investigate theoretical, laboratory, and atmospheric evidence for a
      recently proposed hypothesis: homogenous ice nucleation occurs at the surface, not in the volume, of supercooled water drops. Using existing
      thermodynamic arguments, laboratory experiments, and atmospheric data, we conclude that ice embryo formation at the surface cannot be confirmed or
      disregarded. Ice nucleation rates measured as a function of drop size in an
      air ambient could help distinguish between volume and surface nucleation rates.</abstract>
	<references>
	</references>
</article>

