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In this supplementary article to Kostinkskiy et al. (2020), we evaluate howit is possible to initiate and synchronize the start of a large number ofstreamer flashes, which can provide a powerful VHF signal, in the time range of~1-3 us. As described in Kostinskiy et al. (2020), we will assume streamerflashes occur due to the voluminous network of 'air electrode' (Eth-volumes),the number of which is dynamically supported in highly turbulent regions of athundercloud until an extensive air shower (EAS) passes through this region.The first numerical estimates are given herein. In the near future we plan aseparate article based on these estimates, where we will present the mainpoints in more detail.

Calculation of the dynamics of the initiation of streamer flashes that  provide the NBE VHF signal profile and the VHF phase wave propagation  velocity