Publication:
Very low latitude (L=1.08) whistlers

dc.contributor.coauthorSingh, Rajesh
dc.contributor.coauthorCohen, Morris B.
dc.contributor.coauthorMaurya, Ajeet K.
dc.contributor.coauthorVeenadhari, B.
dc.contributor.coauthorKumar, Sushil
dc.contributor.coauthorPant, P.
dc.contributor.coauthorSaid, Ryan K.
dc.contributor.departmentDepartment of Electrical and Electronics Engineering
dc.contributor.kuauthorİnan, Umran Savaş
dc.contributor.schoolcollegeinstituteCollege of Engineering
dc.date.accessioned2024-11-09T13:13:40Z
dc.date.issued2012
dc.description.abstractFor decades, whistlers observed on the ground at mid and high latitudes have been used for diagnostics of Earth's plasmasphere. Whistlers have also been observed at low latitudes however, the propagation characteristics of low latitude whistlers are poorly understood thus they have not been used effectively as a diagnostic for the low latitude ionosphere. One key limitation with past studies has been lack of knowledge of the whistler source lightning location. Here we present the first cases of low latitude ground whistlers most likely linked with their causative lightning discharges in the conjugate zone. The Global Lightning Dataset 360 (GLD360) detected lightning discharges were found to be located close to the conjugate location of the recording stations, providing direct evidence of interhemispheric propagation at the low latitudes. A total of 864 whistlers were observed at Allahabad, India (Geomag. lat. 16.05 degrees N; Geomag. long. 155.34 degrees E; L = 1.08) during the night of 26 January 2011. Using GLD360 network data, we show the occurrence of thunderstorm activity between 200 and 450 km from the conjugate point of Allahabad. We also report the distribution of peak currents of whistler-producing lightning, which demonstrate a cutoff at 30 kA. Citation: Singh, R., M. B. Cohen, A. K. Maurya, B. Veenadhari, S. Kumar, P. Pant, R. K. Said, and U. S. Inan (2012), Very low latitude (L = 1.08) whistlers, Geophys. Res. Lett., 39, L23102, doi: 10.1029/2012GL054122.
dc.description.fulltextYES
dc.description.indexedbyWOS
dc.description.indexedbyScopus
dc.description.issue23
dc.description.openaccessYES
dc.description.publisherscopeInternational
dc.description.sponsoredbyTubitakEuN/A
dc.description.sponsorshipIndian Institute of Geomagnetism (IIG)
dc.description.sponsorshipIndo-U.S. Science and Technology Forum (IUSSTF)
dc.description.sponsorshipAFRL
dc.description.sponsorshipCAWSES India, Phase-II program
dc.description.versionPublisher version
dc.description.volume39
dc.identifier.doi10.1029/2012GL054122
dc.identifier.embargoNO
dc.identifier.filenameinventorynoIR00106
dc.identifier.issn0094-8276
dc.identifier.quartileQ1
dc.identifier.scopus2-s2.0-84870865266
dc.identifier.urihttps://doi.org/10.1029/2012GL054122
dc.identifier.wos312094400002
dc.keywordsPropagation
dc.keywordsExcitation
dc.keywordsLightning discharge
dc.keywordsWhistlers
dc.language.isoeng
dc.publisherAmerican Geophysical Union (AGU)
dc.relation.grantnoFA9453-11-C-0011
dc.relation.ispartofGeophysical Research Letters
dc.relation.urihttp://cdm21054.contentdm.oclc.org/cdm/ref/collection/IR/id/1138
dc.subjectGeosciences
dc.subjectMultidisciplinary
dc.titleVery low latitude (L=1.08) whistlers
dc.typeJournal Article
dspace.entity.typePublication
local.contributor.kuauthorİnan, Umran Savaş
local.publication.orgunit1College of Engineering
local.publication.orgunit2Department of Electrical and Electronics Engineering
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