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<article language="en">
	<journal>
		<journal_title>Advances in Science and Research</journal_title>
		<journal_url>www.adv-sci-res.net</journal_url>
		<issn>1992-0628</issn>
		<eissn>1992-0636</eissn>
		<volume_number>3</volume_number>
		<volume_title>8th EMS Annual Meeting and 7th European Conference on Applied Climatology 2008</volume_title>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/asr-3-17-2009</doi>
	<article_url>http://www.adv-sci-res.net/3/17/2009/</article_url>
	<abstract_html>http://www.adv-sci-res.net/3/17/2009/asr-3-17-2009.html</abstract_html>
	<fulltext_pdf>http://www.adv-sci-res.net/3/17/2009/asr-3-17-2009.pdf</fulltext_pdf>
	<start_page>17</start_page>
	<end_page>21</end_page>
	<publication_date>2009-04-02</publication_date>
	<article_title content_type="html">Tornado funnel-shaped cloud as convection in a cloudy layer</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. V. Zavolgenskiy</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>P. B. Rutkevich</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Water Problems Institute RAN, South Department, RAN, 198 Stachka av., Rostov-on-Don, Russia</affiliation>
		<affiliation numeration="2" content_type="html">Space Research Institute (IKI) RAN, Moscow, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">Analytical model of convection in a thick horizontal cloud layer with free
upper and lower boundaries is constructed. The cloud layer is supposed to be
subjected to the Coriolis force due to the cloud rotation, which is a typical
condition for tornado formation. It is obtained that convection in such
system can look as just one rotating cell in contrast to the usual many-cells
Benard convection. The tornado-type vortex is different from spatially periodic
convective cells because their amplitudes vanish with distance from the vortex
axis. The lower boundary at this convection can substantially move out of the
initially horizontal cloud layer forming a single vertical vortex with intense
upward and downward flows.  The results are also applicable to convection in
water layer with negative temperature gradient.</abstract>
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</article>

