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Fig. 9 | Earth, Planets and Space

Fig. 9

From: Effects of shallow-layer reverberation on measurement of teleseismic P-wave travel times for ocean bottom seismograph data

Fig. 9

Top synthetic seismograms for the two shallow-layer models shown in Table 3. Bottom synthetic seismograms for the two shallow-layer models after cross-convolving the responses for each other’s shallow-layer structure. Waveforms for the AK135 model are shown in black and waveforms for the seafloor model are shown in red via time shifting by the ray theoretical travel time difference between the two shallow-layer models and by broken blue lines at times of maximum correlation with synthetics for the AK135 model. Bandpass filter is applied at a central period of (a, f) 2.7, (b, g) 5.3, (c, h) 7.5 (d, i), 10.6 and (e, j) 21.2 s

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