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- W2017752526 abstract "The radar cross section of a cloud-to-ground lightning stroke is calculated for the two limiting cases of overdense and underdense plasma. By using a model of the decaying channel and smoothly joining these limiting cases, curves of the temporal variation of the radar cross section can be obtained. Results are presented for wavelengths of 3.2, 10, 23, and 150 cm. Comparison with radar noise levels shows that radars of wavelength 10 cm or greater can be used to monitor the conditions within lightning strokes for up to about 100 msec after stroke incidence. Radars with wavelengths much less than 10 cm are not so suitable. With radar it should be possible to determine the lightning channel conditions conducive to dart leader formation, the relationship between initial ionization density and dart leader speed, the ratio of the diameters of leaders and return strokes, some information on the electron density inside leaders and its temporal variation, and also, with radars of smaller wavelength, (3 cm or less) the initial shock expansion rate of the return stroke. The radar cross section of the dielectric discontinuity of the hot air of the channel is shown to be negligible, in agreement with Browne (1951)." @default.
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- W2017752526 date "1972-08-20" @default.
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- W2017752526 title "Radar as a diagnostic tool for lightning" @default.
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- W2017752526 doi "https://doi.org/10.1029/jc077i024p04518" @default.
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