Abstract

Discovered the effects of regular solar and geodynamic fluctuations in satellite data on the insolation falling on the earth's surface at the point of the Kara-Dag for the period 1983.5 in 2005.5 years. The parameters of the seasonal component are determined. Possible reasons for the increase in the amplitude of the seasonal component are discussed.

Highlights

  • To explore emerging and developing deformation processes, movements of lithospheric plates are created geodynamic polygons, experimental equipment, which implements the comprehensive observational techniques of radio interferometry with very long base (VLBI), laser ranging to artificial satellites (LRS) satellite systems GPS and GLONASS

  • To explore emerging and developing deformation processes, movements of lithospheric plates are created geodynamic polygons, equipped with high-precision experimental equipment, which is implemented to conduct comprehensive observational methods radiointerferometry with very long base (VLBI), laser ranging to artificial satellites (LRS) satellite systems GPS and GLONASS

  • The position of Crimea near the rift of the Eurasian plate and the increased development of the Peninsula building complexes requires the creation of an integrated network of local geodynamic stations, prediction capabilities, and environmental safety for carrying out geodetic, construction and agricultural works

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Summary

Introduction

To explore emerging and developing deformation processes, movements of lithospheric plates are created geodynamic polygons, experimental equipment, which implements the comprehensive observational techniques of radio interferometry with very long base (VLBI), laser ranging to artificial satellites (LRS) satellite systems GPS and GLONASS. One of the main objectives of helio-geodynamic research based on geodetic and space-based measurements is to create and maintain catalogs and maps the rates of change of deformation of the earth's surface. Deformation and movement of the plate over long periods of time and have had currently effect on improvement of processes inside the earth (earthquakes, volcanoes, mudslides). The activation inside the earth processes is indicated by anomalies in the displacement of the surface of observation points. The description of longterm changes and prediction of geophysical and climatic characteristics of the Peninsula are possible on continuous ground-based observations over many years

Monitoring of deformation processes
Conclusion
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