Abstract
This paper studies the importance of spatial distribution of the sea-level monitoring stations for the accuracy of restoration of a tsunami source. The ill-posed inverse restoration problem is regularized by means of the least squares inversion using a truncated SVD approach. The wave propagation is described by linearized shallow-water equations when depth depends on an arbitrary function of two variables. Results of numerical experiments are presented in the case study of the Peru coastal area.
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voronina.pdf498.07 KB
Pages
83-91