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The excitation of tsunami by low-frequency nonstationary point and distributed centres of expansion - MaRDI portal

The excitation of tsunami by low-frequency nonstationary point and distributed centres of expansion (Q2761369)

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scientific article; zbMATH DE number 1683412
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English
The excitation of tsunami by low-frequency nonstationary point and distributed centres of expansion
scientific article; zbMATH DE number 1683412

    Statements

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    18 December 2001
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    tsunami
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    source oscillation
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    elastic bottom
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    ocean surface elevation
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    low-frequency oscillation
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    The excitation of tsunami by low-frequency nonstationary point and distributed centres of expansion (English)
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    The authors propose a model of ocean in which at a depth of 40 km under the elastic bottom a point or a distributed expansion center acts causing the elevation of the bottom. The authors study the dependence of the ocean surface elevation on the oscillatory action of the expansion center. It is established that observable tsunami can be caused only by low-frequency oscillations of the source.
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