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ELF sferic energy as a proxy indicator for sprite occurrence

dc.contributor.authorInan, Umran S., author
dc.contributor.authorReising, Steven C., author
dc.contributor.authorBell, Timothy F., author
dc.contributor.authorAmerican Geophysical Union, publisher
dc.date.accessioned2007-01-03T08:10:56Z
dc.date.available2007-01-03T08:10:56Z
dc.date.issued1999
dc.description.abstractBroadband ELF/VLF measurements of sferics near Ft. Collins, Colorado, demonstrate that ELF sferic energy is a proxy for sprite occurrence which can be used to estimate the number of sprites produced by a thunderstorm. Ultra-long range (~12,000 km) measurements at Palmer Station, Antarctica, confirm the application of this proxy to storms where no video observations of sprites are available. Comparison with high-resolution photometer measurements demonstrate the simultaneity of sprite luminosity and an ELF "second pulse" believed to be radiated by electrical currents within the sprite body [Cummer et al., 1998]. Measurements of the second ELF pulse are used to identify a quantitative relationship between the current in sprites and total sprite luminosity.
dc.format.mediumborn digital
dc.format.mediumarticles
dc.identifier.bibliographicCitationResiing, Steven C., Umran S. Inan, and Timothy F. Bell, ELF Sferic Energy as a Proxy Indicator for Sprite Occurrence, Geophysical Research Letters 26, no. 7 (April 1, 1999): 987-990.
dc.identifier.urihttp://hdl.handle.net/10217/68071
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relation.ispartofFaculty Publications
dc.rights©1999 American Geophysical Union.
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.titleELF sferic energy as a proxy indicator for sprite occurrence
dc.typeText

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