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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>2</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/acpd-2-689-2002</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/2/689/2002/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/2/689/2002/acpd-2-689-2002.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/2/689/2002/acpd-2-689-2002.pdf</fulltext_pdf>
	<start_page>689</start_page>
	<end_page>714</end_page>
	<publication_date>2002-06-12</publication_date>
	<article_title content_type="html">A condensed-mass advection based model for the simulation of liquid polar stratospheric clouds</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Lowe</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. R. MacKenzie</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>N. Nikiforakis</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>J. Kettleborough</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Lancaster University, United Kingdom</affiliation>
		<affiliation numeration="2" content_type="html">DAMTP, Cambridge University, United Kingdom</affiliation>
		<affiliation numeration="3" content_type="html">Rutherford Appleton Laboratory, United Kingdom</affiliation>
	</affiliations>
	<abstract content_type="html">We present a condensed-mass advection based model (MADVEC) designed to
      simulate the condensation/evaporation of liquid polar stratospheric cloud
      (PSC) particles. A (Eulerian-in-radius) discretization scheme is used, making
      the model suitable for use in global or mesoscale chemistry and transport models
      (CTMs). The mass advection equations are solved using an adaption of the weighted average flux (WAF) scheme. We validate the numerical scheme
      using an analytical solution for multicomponent aerosols. The physics of the
      model are tested using a test case designed by Meilinger
      et al. (1995). The results from this test corroborate the composition gradients across the size
      distribution under rapid cooling conditions that were reported in earlier studies.&lt;/p&gt;</abstract>
	<references>
	</references>
</article>

