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<article language="en">
	<journal>
		<journal_title>Advances in Geosciences</journal_title>
		<journal_url>www.adv-geosci.net</journal_url>
		<issn>1680-7340</issn>
		<eissn>1680-7359</eissn>
		<volume_number>25</volume_number>
		<volume_title>Precipitation: Measurement, Climatology, Remote Sensing, and Modeling (EGU Session 2009)</volume_title>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/adgeo-25-71-2010</doi>
	<article_url>http://www.adv-geosci.net/25/71/2010/</article_url>
	<abstract_html>http://www.adv-geosci.net/25/71/2010/adgeo-25-71-2010.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/25/71/2010/adgeo-25-71-2010.pdf</fulltext_pdf>
	<start_page>71</start_page>
	<end_page>77</end_page>
	<publication_date>2010-03-16</publication_date>
	<article_title content_type="html">Heat and energy fluxes in the convective cell behind a cold front</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Ivanov</name>
			<email>svvivo@te.net.ua</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Palamarchuk</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Meteorology and Forecasting, Environmental University, 65016 Odessa, Ukraine</affiliation>
	</affiliations>
	<abstract content_type="html">High resolution model simulations are used to estimate
heat fluxes and energy conversion in the convective cell developing behind a
cold front. It is found that the model is able to simulate rapid temperature
changes in the low troposphere up to 1 &amp;deg;C for a time period of a few
minutes due to latent heat release as well as horizontal acceleration up to
5 m/s at the top of convective circulation. Numerical experiments have also
shown sensitivity of fine resolution simulations to parameterizations used
for the description of a large-scale flow.</abstract>
	<references>
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</article>

