Phase and amplitude perturbations (Trimpis) on man-made VLF signals pr
opagating in the Earth-ionosphere waveguide, due to lightning-induced
ionization occurring off the great circle path from VLF transmitter to
receiver, are sensitive to the instantaneous lateral location of this
ionization. High-altitude winds of similar to 100 m/s can move this i
onization fast enough during its decay to change the rate, shape, and
even sign of the phase and amplitude perturbation decays.