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Characteristics and conditions of production of TLEs observed over a maritime storm

dc.contributor.authorSoula, Serge
dc.contributor.authorVan der Velde, Oscar Arnoud
dc.contributor.authorPalmiéri, J.
dc.contributor.authorChanrion, Olivier
dc.contributor.authorMontañá Puig, Juan
dc.contributor.authorLefeuvre, F.
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria Elèctrica
dc.date.accessioned2010-06-01T08:32:07Z
dc.date.available2010-06-01T08:32:07Z
dc.date.issued2009
dc.identifier.citationSoula, S. [et al.]. Characteristics and conditions of production of TLEs observed over a maritime storm. A: AGU Chapman Conference on Effects of Thunderstorms and Lightning in the Upper Atmosphere. "AGU Chapman Conference on Effects of Thunderstorms and Lightning in the Upper Atmosphere". 2009,
dc.identifier.urihttp://hdl.handle.net/2117/7453
dc.description.abstractThe coordinated European campaign of TLE observation in 2007 involved several cameras in southern France and northern Spain and lasted several months of summer, fall, and winter. Thanks to good conditions of observation at the camera locations and to several periods of long-duration storm activity, a large proportion of the TLEs (~90%) were observed from October to January over the Mediterranean Sea. Different types of TLEs (sprites, halos, elves) were produced by these maritime storms.
dc.format.extent1 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Enginyeria electrònica
dc.subject.lcshThunderstorms
dc.titleCharacteristics and conditions of production of TLEs observed over a maritime storm
dc.typeConference lecture
dc.subject.lemacTempestats
dc.relation.publisherversionhttp://www.agu.org/meetings/chapman/2009/bcall/abstract_presenters.html
dc.rights.accessRestricted access - author's decision
local.identifier.drac2510973
dc.description.versionPreprint
local.citation.contributorAGU Chapman Conference on Effects of Thunderstorms and Lightning in the Upper Atmosphere
local.citation.publicationNameAGU Chapman Conference on Effects of Thunderstorms and Lightning in the Upper Atmosphere


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