Characteristics of a Negative Cloud-to-Ground Lightning Discharge Based on Locations of VHF Radiation Sources
SUN Zhu-Ling1,2, QIE Xiu-Shu1, LIU Ming-Yuan1
Figure 1 The very high frequency VHF radiation field detected by the short-baseline time-difference of arrival TDOA location system and simultaneous electric field changes of the lightning recorded by the fast and slow antennas. R indicates the return stroke and K1-K6 indicate the six K processes.