Mostra el registre d'ítem simple

dc.contributor.authorRutledge, Steven A.
dc.contributor.authorLang, Timothy J.
dc.contributor.authorCohen, Morris B.
dc.contributor.authorVan der Velde, Oscar Arnoud
dc.contributor.authorMacGorman, Donald R.
dc.contributor.authorBeasley, William
dc.contributor.authorStanley, Mark A.
dc.contributor.authorLu, Gaopeng
dc.contributor.authorCummer, Steven A.
dc.contributor.authorLyons, Walter A.
dc.contributor.authorKrehbiel, Paul R.
dc.contributor.authorLi, Jingbo
dc.contributor.authorRison, William
dc.contributor.authorThomas, Ronald J.
dc.contributor.authorEdens, Harald E.
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria Elèctrica
dc.date.accessioned2011-11-21T15:48:49Z
dc.date.available2011-11-21T15:48:49Z
dc.date.created2011-06-21
dc.date.issued2011-06-21
dc.identifier.citationLu, G. [et al.]. Lightning development associated with two negative gigantic jets. "Geophysical research letters", 21 Juny 2011, vol. 38, núm. L12801, p. 1-6.
dc.identifier.issn0094-8276
dc.identifier.urihttp://hdl.handle.net/2117/13993
dc.description.abstractWe report observations of two negative polarity gigantic jets sufficiently near very high‐frequency (VHF) lightning mapping networks that the associated lightning characteristics and charge transfer could be investigated. In both cases the gigantic jet‐producing flash began as ordinary intracloud lightning with upper level channels attempting to exit the cloud, and then produced the upward gigantic jet. Neither flash had developed channels to ground, confirming that the major charge transfer during gigantic jets occurred between the cloud and ionosphere. The leader progression of one event was detected at altitudes above 20 km, demonstrating the possibility of detecting and tracking the propagation of negative jets above the cloud with VHF techniques.
dc.format.extent6 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Energies::Energia elèctrica
dc.subject.lcshAtmospheric electricity -- Research
dc.titleLightning development associated with two negative gigantic jets
dc.typeArticle
dc.subject.lemacElectricitat atmosfèrica
dc.identifier.doi10.1029/2011GL047662
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttp://www.agu.org/pubs/crossref/2011/2011GL047662.shtml
dc.rights.accessRestricted access - publisher's policy
local.identifier.drac5837788
dc.description.versionPostprint (published version)
local.citation.authorLu, G.; Cummer, S.; Lyons, W.; Krehbiel, P.; Li, J.; Rison, W.; Thomas, R.; Edens, H.; Stanley, M.; Beasley, W.; MacGorman, D.; Van der Velde, O.A.; Cohen, M.; Lang, T.; Rutledge, S.
local.citation.publicationNameGeophysical research letters
local.citation.volume38
local.citation.numberL12801
local.citation.startingPage1
local.citation.endingPage6


Fitxers d'aquest items

Imatge en miniatura

Aquest ítem apareix a les col·leccions següents

Mostra el registre d'ítem simple