Lunar–solar tide effects in the Earth’s crust and atmosphere
- Authors: Adushkin V.V.1, Riabova S.A.1, Spivak A.A.1
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Affiliations:
- Institute of Geosphere Dynamics
- Issue: Vol 53, No 4 (2017)
- Pages: 565-580
- Section: Article
- URL: https://journal-vniispk.ru/1069-3513/article/view/224161
- DOI: https://doi.org/10.1134/S1069351317040012
- ID: 224161
Cite item
Abstract
The gravitational interaction in the Earth–Moon–Sun system is considered from the standpoint of influencing the formation of time variations in the geophysical fields and some natural processes. The analysis of the results of instrumental observations revealed the main periodicities and cycles in the time variations of subsoil radon volumetric activity with the same periods as the vertical component of the variations of the tidal force. The amplitude modulation of seismic noise by the lunar-solar tide is demonstrated. It is shown that the intensity of relaxation processes in the Earth’s crust has a near-diurnal periodicity, whereas the spectrum of groundwater level fluctuations includes clearly expressed tidal waves. Based on the data on the tilts of the Earth’s surface, the role of tidal deformation in the formation of the block motions in the Earth’s crust is analyzed. A new approach is suggested for identifying tidal waves in the atmosphere by analyzing micropulsations of the atmospheric pressure with the use of adaptive rejection filters.
About the authors
V. V. Adushkin
Institute of Geosphere Dynamics
Email: spivak@idg.chph.ras.ru
Russian Federation, Moscow
S. A. Riabova
Institute of Geosphere Dynamics
Email: spivak@idg.chph.ras.ru
Russian Federation, Moscow
A. A. Spivak
Institute of Geosphere Dynamics
Author for correspondence.
Email: spivak@idg.chph.ras.ru
Russian Federation, Moscow
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