Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity

We analyzed what kind of fundamental physical phenomena can be responsible for the generation of the anomalous latitudinal zones of the seismic activity, and the hotspots, and some other geophysical processes. The assessment of tidal effect contribution to the earthquake preparation process is discu...

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Bibliographic Details
Main Authors: B. Levin, A. Domanski, E. Sasorova
Format: Article
Language:English
Published: Copernicus Publications 2014-01-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/35/137/2014/adgeo-35-137-2014.pdf
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Summary:We analyzed what kind of fundamental physical phenomena can be responsible for the generation of the anomalous latitudinal zones of the seismic activity, and the hotspots, and some other geophysical processes. The assessment of tidal effect contribution to the earthquake preparation process is discussed. A disk model of the Earth's rotation was proposed. The model is acceptable for the homogeneous Earth and for the heterogeneous one. The disk model explains the nucleation of two maximums of the gradient of the moment of inertia over latitude with respect to the Equator. Effects of the variations in the Earth's rotation angular velocity were estimated and the possible features caused by the rotation velocity instability were described. The variations in the relative velocity of the Earth's rotation (dimensionless value ν ≈ (<i>T</i> − <i>P)/P</i>) are approximately equal upon the average to 10<sup>&minus;8</sup>, where <i>T</i> is the observed length of day for the Earth, and <i>P</i> is the astronomical day. These variations lead to the occurrence of the additional energy estimated as 10<sup>20</sup> J. <br><br> The authors proposed the hypothesis of a pulsating geoid based on effects of the Earth's rotation features, and tidal forces, and conception of critical latitudes in the solid Earth. This hypothesis may highlight the phenomenon of zonal intensification of some geological processes in the solid Earth (the seismic activity, and hotspot location, and major ore deposit locations).
ISSN:1680-7340
1680-7359