Electromagnetic Model of K‐Changes

K‐changes are observed as step‐like increases in the thundercloud electric fields. The K‐changes occur in the late part of intra‐cloud lightning or during negative cloud‐to‐ground lightning between return strokes. It has been shown that the processes leading to K‐changes initiate in the decayed part...

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Veröffentlicht in:	Journal of geophysical research. Atmospheres 2024-10, Vol.129 (20), p.n/a
Hauptverfasser:	Kašpar, Petr, Marshall, Thomas, Stolzenburg, Maribeth, Kolmašová, Ivana, Santolík, Ondřej
Format:	Artikel
Sprache:	eng
Schlagworte:	Amplitudes Conductivity Electric charge Electric field Electric fields Electric potential Electrostatic properties intra‐cloud process K‐change Leader currents Lightning Maxwell's equations Measuring instruments Poisson equation Poisson's equation Propagation velocity Pulse propagation Return stroke Return strokes (lightning) Wave fronts Waveforms
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