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The figure illustrates the calculation of an airplane's true ground velocity.
Energy in an earthquake passing a particular surface site can be calculated directly from the recordings of seismic ground motion, given, for example, as ground velocity.
peak ground velocity.
Upper vertical ground velocity (m/s).
Fig. 3 (a) Ground velocity record of an artificial earthquake during a blasting experiment and (b) electric field record, corresponding to the ground velocity.
Fig. 4 (a) Ground velocity record of another artificial earthquake during another blasting experiment at another site and (b) electric field record, corresponding to the ground velocity.
The maximum observed ground velocity is shown at the beginning of each waveform.
Traces indicate ground velocity, and scales are shown on the right corners of each trace.
To estimate the arrival direction, we need to know ground velocity, displacement, and its spatial derivatives.
The magnitude of generated electric field is obviously proportional to the magnitude of ground velocity.
In Fig. 4(a), the polarity of ground velocity was found to be reversed.
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CEO of Professional Science Editing for Scientists @ prosciediting.com