“…Because varies generally smoothly, its effect on the phase of the signal is muted, which explains the success of previous travel time‐based analyses, using both local and teleseismic earthquakes or ambient seismic field directly with DAS strain recordings (Yu et al, ; Zeng et al, ). Because body waves have almost no dispersion, DAS measurements allow measurement of their travel times directly from strain records (e.g., Lellouch et al, , ; Lellouch, Yuan, et al, ).…”