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Martian Infrasound: Numerical Modeling and Analysis of InSight's Data

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Academic year: 2021

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Figure 1 illustrates the inertial effects by presenting compliance estimates for three sub-surface models and various atmospheric horizontal speeds
Figure 2. a) Average values of vertical compliance of atmospheric pressure perturbations normalized to wind speed (in 1/Pa) as a function of frequency (in Hz), estimated through  compli-ance measurements using the VEL outputs of SEIS-VBB sensors (Garcia et
Figure 3. Synthetics of the full-wave simulation discussed in Section 4.2. Left: time-distance plots of synthetic ground pressure perturbations, shown in two directions on the same plot
Figure 4. Characterization of ground-recorded pressure perturbation ∆P and subsequent ground movements V h,z , from synthetics
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