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dc.contributor.authorLointier, G.
dc.contributor.authorLefeuvre, F.
dc.contributor.authorSoula, Serge
dc.contributor.authorVan der Velde, Oscar Arnoud
dc.contributor.authorPalmiéri, J.
dc.contributor.authorChanrion, Olivier
dc.contributor.authorNeubert, Torsten
dc.contributor.authorMontañá Puig, Juan
dc.contributor.authorGangneron, F.
dc.contributor.authorMeyerfeld, Y.
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria Elèctrica
dc.date.accessioned2010-09-13T12:53:55Z
dc.date.available2010-09-13T12:53:55Z
dc.date.created2010-07-08
dc.date.issued2010-07-08
dc.identifier.citationSoula, S. [et al.]. Characteristics and conditions of production of transient luminous events observed over a maritime storm. "Journal of Geophysical Research", 08 Juliol 2010, vol. 115, p. 16118-16132.
dc.identifier.urihttp://hdl.handle.net/2117/8837
dc.description.abstractOn the night of 15/16 November 2007, cameras in southern France detected 30 transient luminous events (TLEs) over a storm located in the Corsican region (France). Among these TLEs, 19 were sprites, 6 were halos, and 5 were elves. For 26 of them, a positive “parent” cloud-to-ground lightning (P+CG) flash was identified. The peak current of the P+CG flashes for the sprites had an average value of 63 kA and had a maximum value of 125 kA. The flashes for the halos and the elves had average values of 272 and 351 kA, respectively, and they had maximum values of 312 and 384 kA, respectively. No TLEs were detected after negative CG flashes with very large peak currents. Among the 26 P+CG flashes, 23 were located in a stratiform region with reflectivity values lower than 45 dBZ. The CG flashes in this region were classified into two groups according to the time interval separating them from the following flash: one group with values less than 2 s and one with values greater than 2 s. About 79% of all CGs were produced in a sequence of at least two flashes less than 2 s apart. For 65.5% of the sequences, the first flash was positive with an average peak current of 73 kA, while the later +CG flashes in a sequence had much lower peak currents. Several triangulated sprites were found to be shifted from their P+CG flashes by about 10 to 50 km and preferentially downstream. The observations suggest that the P+CG flashes can initiate both sprites and other CG flashes in a storm.
dc.format.extent15 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Enginyeria de la telecomunicació::Radiocomunicació i exploració electromagnètica
dc.subject.lcshTransient luminous event
dc.subject.lcshTLE
dc.titleCharacteristics and conditions of production of transient luminous events observed over a maritime storm
dc.typeArticle
dc.subject.lemacElectricitat atmosfèrica
dc.identifier.doi10.1029/2009JD012066
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttp://www.agu.org/
dc.rights.accessRestricted access - publisher's policy
local.identifier.drac2642231
dc.description.versionPostprint (author’s final draft)
local.citation.authorSoula, S.; Van der Velde, O.A.; Palmiéri, J.; Chanrion, O.; Neubert, T.; Montaña, J.; Gangneron, F.; Meyerfeld, Y.; Lefeuvre , F.; Lointier, G.
local.citation.publicationNameJournal of Geophysical Research
local.citation.volume115
local.citation.startingPage16118
local.citation.endingPage16132


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