Electric field intensity of the lightning return stroke
1973; American Geophysical Union; Volume: 78; Issue: 18 Linguagem: Inglês
10.1029/jc078i018p03523
ISSN2156-2202
AutoresM. A. Uman, D. Kenneth McLain, Richard J. Fisher, E. Philip Krider,
Tópico(s)Electromagnetic Compatibility and Noise Suppression
ResumoJournal of Geophysical Research (1896-1977)Volume 78, Issue 18 p. 3523-3529 Electric field intensity of the lightning return stroke Martin A. Uman, Martin A. UmanSearch for more papers by this authorD. Kenneth McLain, D. Kenneth McLainSearch for more papers by this authorRichard J. Fisher, Richard J. FisherSearch for more papers by this authorE. Philip Krider, E. Philip KriderSearch for more papers by this author Martin A. Uman, Martin A. UmanSearch for more papers by this authorD. Kenneth McLain, D. Kenneth McLainSearch for more papers by this authorRichard J. Fisher, Richard J. FisherSearch for more papers by this authorE. Philip Krider, E. Philip KriderSearch for more papers by this author First published: 20 June 1973 https://doi.org/10.1029/JC078i018p03523Citations: 35AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Abstract From an examination of about 1000 electric field wave forms produced by lightning return strokes in 16 storms at distances between 20 and 100 km from an observation site at the Kennedy Space Center, Florida, a typical return stroke current wave form is derived. For this current wave form, the electric field intensity at distances between 0.5 and 100 km is computed for three values of return stroke velocity. The resultant curves for close lightning are compared with measured field wave forms. The transmission line return stroke model is used in all calculations since, as discussed, the Bruce-Golde model cannot account for the observed electric field characteristics. References Bruce, C. E. R., R. H. Golde, The lightning discharge, J. Inst. Elec. Eng. Part 2, 88, 487– 524, 1941. Dennis, A. S., E. T. Pierce, The return stroke of a lightning flash to earth as a source of VLF atmospherics, Radio Sci., 68D, 777– 794, 1964. Fisher, R. J., M. A. Uman, Measured electric field rise times for first and subsequent lightning return strokes, J. Geophys. Res., 77, 399– 406, 1972. McLain, D. K., M. A. Uman, Exact expression and moment approximation for the electric field intensity of the lightning return stroke, J. Geophys. Res., 76, 2101– 2105, 1971. Morrison, R. B., The variation with distance in the range 0–100 km of atmospheric wave-forms, Phil. Mag., 44, 980– 992, 1953. Schonland, B. F. J., The lightning discharge, Handb. Phys., 22, 576– 628, 1956. Schonland, B. F. J., D. J. Malan, H. Collens, Progressive lightning, 2, Proc. Roy. Soc., Ser. A, 152, 595– 625, 1935. Taylor, W. L., Radiation field characteristics of lightning discharges in the band 1 kc/s to 10 kc/s, Radio Sci., 67D, 539– 550, 1963. Uman, M. A., Lightning, 69, McGraw-Hill, New York, 1969. Uman, M. A., D. K. McLain, Magnetic field of lightning return stroke, J. Geophys. Res., 74, 6899– 6910, 1969. Uman, M. A., D. K. McLain, Lightning return stroke current from magnetic and radiation field measurements, J. Geophys. Res., 75, 5143– 5147, 1970a. Uman, M. A., D. K. McLain, Radiation field and current of the lightning stepped leader, J. Geophys. Res., 75, 1058– 1066, 1970b. Uman, M. A., D. K. McLain, R. J. Fisher, E. P. Krider, Currents in Florida lightning return strokes, J. Geophys. Res., 7818, 1973. Citing Literature Volume78, Issue18Oceans and Atmospheres20 June 1973Pages 3523-3529 ReferencesRelatedInformation
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