Generation of microseisms in the coastal area

Details Generation of microseisms in the coastal area Generation of microseisms in the coastal area

Oct 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990pepi...63..201g&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 63, Issue 3-4, p. 201-208.

Physics

2

Scientific paper

This paper considers the regularities and properties of microseisms and swell in the coastal area of East Kamchatka. Based on extensive experimental data, dependences were obtained of the value of coastal swell and the amplitude of microseisms on the period. A relationship was revealed between the vertical and horizontal components of microseisms. The dependence of the amplitude of microseisms on the value of swell is non-linear for both the horizontal and vertical components. For the horizontal component, the non-linearity is much more significant.
The mechanism of the generation of horizontal components by bottom friction is considered. Analysis of the hydrodynamic conditions of swell in the coastal area shows the possibility of the generation of vertical and horizontal components by, respectively, bottom pressure and bottom friction. Estimations were made of the dimensions of the microseismic generation areas in the coastal zone.

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