Synthetic tsunami mareograms for realistic oceanic models

Details Synthetic tsunami mareograms for realistic oceanic models Synthetic tsunami mareograms for realistic oceanic models

May 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000geoji.141..498p&link_type=abstract

Geophysical Journal International, Volume 141, Issue 2, pp. 498-508.

Astronomy and Astrophysics

Astronomy

2

Lateral Heterogeneity, Synthetic Mareograms, Tsunamis

Scientific paper

We study how the tsunami mode is generated by a scaled double-couple seismic source, and how it propagates in realistic oceanic models. The method developed and used is the direct extension to tsunami waves propagating in multilayered oceanic media of the well-known Haskell method. The most intensive tsunamis may be expected from sources located within the crust in the deep-water parts of the ocean. The extension to laterally heterogeneous structures shows that, if the thickness of the ocean liquid layer diminishes, the maximum amplitude of the tsunami wave train increases.

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