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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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>−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>−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 |
work_keys_str_mv |
AT blevin zonalconcentrationofsomegeophysicalprocessintensitycausedbytidesandvariationsintheearthsrotationvelocity AT adomanski zonalconcentrationofsomegeophysicalprocessintensitycausedbytidesandvariationsintheearthsrotationvelocity AT esasorova zonalconcentrationofsomegeophysicalprocessintensitycausedbytidesandvariationsintheearthsrotationvelocity |
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