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b Modeled surface displacement.
(c) Vertical surface displacement associated with the main shock.
Figures 10 and 11 show local surface displacement inferred by InSAR, after the removal of global surface displacement.
The surface displacement is calculated by using the method of Mansinha and Smylie (1971), and the surface displacement is assumed to accomplish in 60 s.
Finally, a surface displacement velocity was estimated by applying a best-fit linear function, assuming a constant velocity for the surface displacement.
Accordingly, our observed spatial heterogeneity of surface displacement cannot be explained by such a mechanism.
Then, we synthesize surface displacement data and analyze them to estimate the slip deficit distribution.
It is normalized to the coseismic surface displacement (s_{mathrm{s}}).
The surface displacement generated by afterslip is shown as a function of time in Fig. 9.
Equation 43 is an integro-differential equation governing the surface displacement η* t).
Fig. 3 Surface displacement of the 1707 Hoei earthquake (Annaka et al., 2003).
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