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<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>9</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-155-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/155/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/155/2009/acp-9-155-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/155/2009/acp-9-155-2009.pdf</fulltext_pdf>
	<start_page>155</start_page>
	<end_page>161</end_page>
	<publication_date>2009-01-12</publication_date>
	<article_title content_type="html">Cloud&apos;s Center of Gravity – a compact approach to analyze convective cloud development</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>I. Koren</name>
			<email>ilan.koren@weizmann.ac.il</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>O. Altaratz</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>G. Feingold</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>Z. Levin</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>T. Reisin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dept. of Environ. Sciences Weizmann Institute, Rehovot, Israel</affiliation>
		<affiliation numeration="2" content_type="html">NOAA Earth System Research Laboratory, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">Dept. of Geophysics and Planetary Sciences, Tel Aviv University, Tel Aviv, Israel</affiliation>
		<affiliation numeration="4" content_type="html">Soreq Nuclear Research Center, Yavne, Israel</affiliation>
	</affiliations>
	<abstract content_type="html">As cloud resolving models become more detailed, with higher resolution
outputs, it is often complicated to isolate the physical processes that
control the cloud attributes. Moreover, due to the high dimensionality and
complexity of the model output, the analysis and interpretation of the
results can be very complicated. Here we suggest a novel approach to
convective cloud analysis that yields more insight into the physical and
temporal evolution of clouds, and is compact and efficient. The different
(3-D) cloud attributes are weighted and projected onto a single point in
space and in time, that has properties of, or similar to, the Center Of
Gravity (COG). The location, magnitude and spread of this variable are
followed in time. The implications of the COG approach are demonstrated for
a study of aerosol effects on a warm convective cloud. We show that in
addition to reducing dramatically the dimensionality of the output, such an
approach often enhances the signal, adds more information, and makes the
physical description of cloud evolution clearer, allowing unambiguous
comparison of clouds evolving in different environmental conditions. This
approach may also be useful for analysis of cloud data retrieved from
surface or space-based cloud radars.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Cotton, W. R., Pielke, R. A., Walko, R. L., Liston, G. E., Tremback, C. J., Jiang, H., McAnelly, R. L., Harrington, J. Y., Nicholls, M. E., Carrio, G. G., and McFadden, J. P.: RAMS 2001: Current status and future directions, Meteo. Atmos. Phys., 82, 5–29, 2003. </reference>
		<reference numeration="2" content_type="text"> Feynman, R., Leighton, R., and Matthew, S.: Center of Mass Moment of Inertia – The Feynman Lectures on Physics, Addison Wesley, Vol 1, Chapter~19, ISBN 0-201-02116-1, 19-1–19-4, 1963. </reference>
		<reference numeration="3" content_type="text"> IPCC: The Intergovernmental Panel on Climate Change (IPCC) website, http://www.ipcc.ch/SPM2feb07.pdf, 2007. </reference>
		<reference numeration="4" content_type="text"> Levin, Z. and Cotton, W. R.: Aerosol Pollution Impact on Precipitation: A Scientific Review, WMO/IUGG International Aerosol Precipitation Science Assessment Group (IAPSAG), 485 pp., 2007. </reference>
		<reference numeration="5" content_type="text"> Meyers, M. P., Walko, R. L., Harrington, J. Y., and Cotton, W. R.: New RAMS cloud microphysics parameterization. Part II: The two-moment scheme., Atmos. Res., 45, 3–39, 1997. </reference>
		<reference numeration="6" content_type="text"> Stephens, G. L., Vane, D. G., Boain, R. J., Mace, G. G., Sassen, K.,, Wang, Z., Illingworth, A. J., O&apos;Connor, E. J., Rossow, W. B., Durden, S. L., Miller, S. D., Austin, R. T., Benedetti, A., and Mitrescu, C.: The cloudsat mission and the a-train, A New Dimension of Space-Based Observations of Clouds and Precipitation, Bull. Am. Meteor. Soc., 83(12), 1771–1790, 2002. </reference>
		<reference numeration="7" content_type="text"> Teller, A. and Levin, Z.: Factorial method as a tool for estimating the relative contribution to precipitation of cloud microphysical processes and environmental conditions: Method and application, J. Geophys. Res., 113, D02202, doi:10.1029/2007JD008960, 2008. </reference>
		<reference numeration="8" content_type="text"> Walko, R., Cotton W. R., Meyers M. P., and Harrington J. Y.,: New RAMS cloud microphysics parameterization. Part I: The single-moment scheme, Atmos. Res. 38, 29–62, 1995. </reference>
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	</references>
</article>

