RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES6003, doi:10.2205/2006ES000212, 2006
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Figure 2 |
[9] Here,
u(x, t) is horizontal velocity component;
h (x, y, t) is perturbation of
the free surface;
H is maximal depth of the basin;
B(x, y, t) is variation in the bottom
of the basin;
H is depth at the 10-meter isobath.
[10] Dynamic seismic source in the form of key-blocks, which can rise (or descend) to a given distance with different velocity, was used for tsunami wave generation [Lobkovsky and Baranov, 1984]. At the initial time moment, parameters of dynamic seismic source (coordinates, velocity of the vertical motion of key-block) are specified in the calculation area. The boundaries are located either in the land regions or the water surface.
Citation: 2006), Numerical modeling of the generation of long waves by a dynamic seismic source and their propagation in the Black Sea, Russ. J. Earth Sci., 8, ES6003, doi:10.2205/2006ES000212.
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