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dc.contributor.authorMezentsev, A.-
dc.contributor.authorLehtinen, N.-
dc.contributor.authorØstgaard, N.-
dc.contributor.authorPérez-Invernón, Francisco J.-
dc.contributor.authorCummer, Steven A.-
dc.date.accessioned2018-05-08T09:27:23Z-
dc.date.available2018-05-08T09:27:23Z-
dc.date.issued2018-
dc.identifierdoi: 10.1002/2017JD027624-
dc.identifierissn: 2169-8996-
dc.identifier.citationJournal of Geophysical Research: Atmospheres 123(1): 139- 159 (2018)-
dc.identifier.urihttp://hdl.handle.net/10261/164523-
dc.description.abstractWe compared the modeled energy spectral density of very low frequency (VLF) radio emissions from terrestrial gamma ray flashes (TGFs) with the energy spectral density of VLF radio sferics recorded by Duke VLF receiver simultaneously with those TGFs. In total, six events with world wide lightning location network (WWLLN) defined locations were analyzed to exhibit a good fit between the modeled and observed energy spectral densities. In VLF range the energy spectral density of the TGF source current moment is found to be dominated by the contribution of secondary low-energy electrons and independent of the relativistic electrons which play their role in low-frequency (LF) range. Additional spectral modulation by the multiplicity of TGF peaks was found and demonstrated a good fit for two TGFs whose VLF sferics consist of two overlapping pulses each. The number of seeding pulses in TGF defines the spectral shape in VLF range, which allows to retrieve this number from VLF sferics, assuming they were radiated by TGFs. For two events it was found that the number of seeding pulses is small, of the order of 10. For the rest of the events the lower boundary of the number of seeding pulses was found to be between 10 to 10.©2017. The Authors.-
dc.description.sponsorshipThis study was supported by the European Research Council under the European Union's Seventh Framework Programme (FP7/2007-2013)/ERC grant agreement 320839 and the Research Council of Norway under contracts 208028/F50 and 223252/F50 (CoE). The contributions of SAC were supported by NSF grant ATM-1565606. The work of FJPI was supported by the Spanish Ministry of Science and Innovation, MINECO under projects ESP2015-69909-C5-2-R and FIS2014-61774-EXP. F.J.P.I. acknowledges a PhD research contract, code BES-2014-069567.-
dc.publisherAmerican Geophysical Union-
dc.relationinfo:eu-repo/grantAgreement/EC/FP7/320839-
dc.relationinfo:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2015-69909-C5-2-R-
dc.relationinfo:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/FIS2014-61774-EXP-
dc.relation.isversionofPublisher's version-
dc.rightsopenAccess-
dc.subjectVLF sferics-
dc.subjectTerrestrial gamma ray flash-
dc.subjectTGF radio emissions-
dc.subjectEarth-ionosphere waveguide-
dc.subjectEIWG propagation-
dc.subjectIC leader-
dc.titleSpectral Characteristics of VLF Sferics Associated With RHESSI TGFs-
dc.typeartículo-
dc.identifier.doi10.1002/2017JD027624-
dc.date.updated2018-05-08T09:27:24Z-
dc.description.versionPeer Reviewed-
dc.language.rfc3066eng-
dc.contributor.funderMinisterio de Ciencia e Innovación (España)-
dc.contributor.funderResearch Council of Norway-
dc.contributor.funderEuropean Research Council-
dc.contributor.funderNational Science Foundation (US)-
dc.relation.csic-
dc.identifier.funderhttp://dx.doi.org/10.13039/100000001es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100004837es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100000781es_ES
dc.identifier.pmid29527426-
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairetypeartículo-
item.grantfulltextopen-
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
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