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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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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spelling doaj-0997f44b644a4ab6b7f8ad17b197a2052020-11-24T22:34:40ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592014-01-013513714410.5194/adgeo-35-137-2014Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocityB. Levin0A. Domanski1E. Sasorova2Institute of Marine Geology and Geophysics, Far East Branch of RAS, Yuzhno-Sakhalinsk, RussiaInstitute of Marine Geology and Geophysics, Far East Branch of RAS, Yuzhno-Sakhalinsk, RussiaShirshov Institute of Oceanology of Russian Academy of Sciences, Moscow, RussiaWe 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).http://www.adv-geosci.net/35/137/2014/adgeo-35-137-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. Levin
A. Domanski
E. Sasorova
spellingShingle B. Levin
A. Domanski
E. Sasorova
Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity
Advances in Geosciences
author_facet B. Levin
A. Domanski
E. Sasorova
author_sort B. Levin
title Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity
title_short Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity
title_full Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity
title_fullStr Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity
title_full_unstemmed Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity
title_sort zonal concentration of some geophysical process intensity caused by tides and variations in the earth's rotation velocity
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2014-01-01
description 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).
url http://www.adv-geosci.net/35/137/2014/adgeo-35-137-2014.pdf
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