Modified Kadomtsev-Petviashvili equation for tsunami over irregular seabed
We derive an asymptotic equation governing the trans-ocean propagation of tsunami from source to the continental shelf. Focus is on disturbances originated from a slender fault of finite length. The variable sea depth is assumed to consist of a slowly varying mean and random fluctuations. The method...
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Format: | Article |
Language: | English |
Published: |
Springer Netherlands,
2016-11-28T20:41:37Z.
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Online Access: | Get fulltext |