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A major issue is to estimate velocity fields in both phases, i.e. liquid and vapor.
An observer is designed for AOBC to estimate velocity and current states of AMB.
There are various methods described in the literature to estimate velocity additions.
Tortuosity as an input parameter in Biot's equation can be used to estimate velocity dispersion.
This paper presents a dynamically compensated velocity observer (DCVO), in which acceleration measurement is employed to estimate velocity.
The sensitivity of the seismic wavefield can also be used to estimate velocity changes in shallow and deep zones separately.
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We estimate velocities at all the stations as follows.
A nonlinear saturated observer is also introduced to estimate velocities of the followers.
We estimate velocities greater than 7.3 km/s within the anomalous body, suggesting that it represents an intrusive plutonic complex.
The sprinkling experiment is used to estimate velocities and celerities, which in turn are used to infer flow pathways.
Simple instrumentation enables thermal and salinity signals to be used to observe flow directions and estimate velocities in these settings.
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