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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>23</volume_number>
		<volume_title>10th EGU Plinius Conference on Mediterranean Storms (2008)</volume_title>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/adgeo-23-11-2010</doi>
	<article_url>http://www.adv-geosci.net/23/11/2010/</article_url>
	<abstract_html>http://www.adv-geosci.net/23/11/2010/adgeo-23-11-2010.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/23/11/2010/adgeo-23-11-2010.pdf</fulltext_pdf>
	<start_page>11</start_page>
	<end_page>16</end_page>
	<publication_date>2010-02-17</publication_date>
	<article_title content_type="html">Prediction of lightning flash density with the WRF model</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>B. Lynn</name>
			<email>yoavya@openu.ac.il</email>
		</author>
		<author numeration="2" affiliations="3">
			<name>Y. Yair</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">The Hebrew University of Jerusalem, Jerusalem, Israel</affiliation>
		<affiliation numeration="2" content_type="html">Weather-It-Is, Efrat, Israel</affiliation>
		<affiliation numeration="3" content_type="html">The Open University of Israel, Ra&apos;anana, Israel</affiliation>
	</affiliations>
	<abstract content_type="html">The Lightning Potential Index (LPI) is a measure of the potential for charge
generation and separation that leads to lightning flashes in convective
thunderstorms. It is calculated from model simulated updraft and
microphysical fields. It was designed to predict the potential of lightning
occurrence in operational weather forecasting models, but could possibly be
used to improve short-range forecasts of heavy rain. The index is modified
here to be model grid-scale transparent between 1 and 4 km (the approximate
upper limit of explicit microphysical weather forecasts). Two case studies
show that the modification appears to work quite well, and that LPI can be
calculated on both an extremely high resolution research-grid (i.e., 1.33 km)
and high resolution (i.e., 4 km) operationally compatible forecast grid.
Analytical expressions are presented to use the LPI to predict the hourly
lightning flash density.</abstract>
	<references>
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</article>

