Fig. 3
From: Infrasound/seismic observation of the Hayabusa reentry: Observations and preliminary results
Infrasound and seismic waveforms (displacement) recorded at GOS2, GOS2A, GOS2B, and GOS2B-sub1 to GOS2B-sub3 stations. Each trace is 5-s long. Dimension of amplitude is Pa for infrasound (P1, P2, and P3) and 10−8 m for ground motion (TS-UD, TS-NS, TS-EW, S1, S2, S3, S4, S5, S6, sub1, sub2, and sub3). Hatched parts of GOS2A are used for array analysis. Enclosed parts of GOS2A TS-UD, TS-NS, and TS-EW traces are used for particle-motion analysis.