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Detection of ground motions using high rate GPS time series

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Figure

Figure 1: Amplitude  vs duration diagram for various geological catastrophic processes
Figure 2: a) The first 15 seconds of the acceleration record of MYG011 strong-motion  site  for  the  M w 9.0  Tohoku  2011  earthquake  and  b)  the  computed  corresponding
Figure 3a: (upper row) Noise level of GPS time-series, compared to (middle row) the  measured  amplitude  of  the  ground  motion  at  10s  and  (lower  row)  at  50s  after  the  origin t0 of the earthquake, based on the Bernese-PPP solution
Figure 3b:  As Figure 2a  for GPS time-series derived  from  solutions of  Wright et al
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