RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES6004, doi:10.2205/2006ES000216, 2006

Figure 12. Dependence of the characteristics of the wave regime at point five
on the accuracy of the algorithm near the boundary and on the size of the grid.
MacCormac scheme of the second order of accuracy (a), Adams scheme with the
second order of approximation at boundary nodes (b), Adams scheme with the
fourth order of approximation at boundary nodes (c). Solid heavy curve:
h0/4 ,
dashed heavy curve:
h0/2 ; solid thin curve:
h0 , dashed line:
2h0.

Citation: Shokin, Yu. I., L. B. Chubarov, Z. I. Fedotova, S. A. Beizel, and S. V. Eletsky (2006), Principles of numerical modeling applied to the tsunami problem, Russ. J. Earth Sci., 8, ES6004, doi:10.2205/2006ES000216.
Copyright 2006 by the Russian Journal of Earth Sciences
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