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In summary, to describe movement the terms velocity and displacement are used; to describe deformation, the terms strain and strain rate are used.
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In any case, even when the optimal velocity trajectory is not affected by some of the forces considered, the optimal control force required to achieve it depends on all the model dynamics (inertial terms, velocity-dependent and static forces).
(Bottom panel) A long-term velocity change and vertical deformation at the Lassen Volcanic Center.
Fig. 5 Short-term velocity vectors derived from a 72-hour sliding window analysis.
(a) Phasor plot of short-term velocity vectors with an exaggerated error interval.
Fig. 8 a A long-term velocity change and vertical deformation at the LVC.
However, there seems to be a long-term velocity perturbation that might be superimposed on the velocity recovery.
These values confirm that fluctuations around the average flow velocity vectors did occur in the short-term velocity vectors.
Furthermore, another constraint focusing on long-term velocity discontinuity across faults has been introduced (Johnson and Fukuda 2010).
After 6 March, the short-term velocity vectors of GPS buoy (W) became irregular and its standard deviations increased.
(d) Autocorrelation analysis of both north-south (NS) and east-west (EW) components of the short-term velocity vectors.
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