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<!DOCTYPE article SYSTEM "http://www.nat-hazards-earth-syst-sci.net/inc/nhess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>5</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/nhess-5-87-2005</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/5/87/2005/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/5/87/2005/nhess-5-87-2005.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/5/87/2005/nhess-5-87-2005.pdf</fulltext_pdf>
	<start_page>87</start_page>
	<end_page>99</end_page>
	<publication_date>2005-01-17</publication_date>
	<article_title content_type="html">Wavelet maxima curves of surface latent heat flux anomalies associated with Indian earthquakes</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Cervone</name>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>R. P. Singh</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Kafatos</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>C. Yu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Center for Earth Observing and Space Research, School of Computational Sciences, George Mason University, Fairfax, VA 22039, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Civil Engineering, Indian Institute of Technology, Kanpur 208 016, India</affiliation>
	</affiliations>
	<abstract content_type="html">Wavelet maxima curves of surface latent heat flux (SLHF) have been
recently used to provide early warning information about coastal earthquakes.
The present paper reports further validations of the spatial and temporal
analysis of wavelet maxima curves associated with earthquakes occurred in
different parts of the Indian sub-continent. Prominent anomalies that exhibit
spatial and temporal continuity are found in case of coastal earthquakes,
while no anomaly is detected in case of intraplate earthquakes. The
precursory SLHF anomalies are found up to 2 weeks prior to the main
earthquake event, with an extent area of up to 600km.</abstract>
	<references>
	</references>
</article>

