Change in the zonal harmonic coefficient C20, Earth’s polar flattening, and dynamical ellipticity from SLR data
Journal Title: Геодинаміка - Year 2018, Vol 25, Issue 2
Abstract
Purpose. We examine the change in the Earth’s second degree zonal harmonic coefficient derived from UTCSR SRL time series of given (a) for the period from 1976 to 2017 as monthly solutions of the zonal coefficient and (b) for the period from 1992 to 2017 as weekly solutions of the zonal coefficient obtained via the eigenvalue-eigenvector problem and related to the principal axes system. The mean difference between the coefficients or given in various systems consists of the value which is smaller than time variations in the coefficients or . These time series of were modeled by polynomials’ different degrees simultaneously with Fourier series with seasonal signals (for annual, semiannual, and quarter-year periods). Final representation was chosen at the epoch J2000 by means of the polynomial of second degree. Then the models for the time-dependent astronomical dynamical ellipticity and the precession constant with respect to the common value were constructed using the model for the zonal coefficient for the time-interval of about 25 yr. As the third step these time series of were applied to determine a basic trend and periodic variations of the time-dependent Earth’s polar flattening from 1992 to 2017. A variation of the global dynamical and geometrical figure of the Earth was investigated and some important quantitative results were found: the polar flattening is increasing within the considered 25 year time-interval. Therefore, this study aims to derive the variation of the global geometrical figure of the Earth, represented by the second-degree coefficients of time-series and the astronomical dynamical ellipticity . As a result, a special attention was given to the study of temporally varying components including seasonal variations of some fundamental parameters of the Earth.
Authors and Affiliations
A. N. Marchenko
Source mechanism and tectonic setting of 29.09.2017 earthquake near Stebnyk
Purpose. The paper’s purpose consists in determining the source mechanism of 29.09.2017 earthquake near Stebnyk (21h46m8.4s, = 49.34˚, λ = 23.49˚, h = 1.9 km, MD = 2.9) using two methods – from polarities of first P-wa...
The stress-strain state modelling of the autochthonous sedimentary complex in the dynamic influence zone of the thrust wedge
Purpose. Computer modelling in the framework of continuum mechanics is a powerful tool to obtain qualitative and quantitative deformation parameters in the geological media. The purpose of this work was to study stress a...
Petrochemical features of the volcanic trappean formation of areas of junction of the volyn paleozoic uplift with the Volyn-Podillya monocline
Goal. Research petrochemical features of volcanites as a precondition for establishing the causes of the localization industry copper-ore mineralization in certain areas strata and suites trappean formation of Western Vo...
Evaluation of three-dimensional deformation fields of the Earth by methods of the projective differential geometry. The main linear deformations
Aim. The aim is to solve the problem of evaluating the Earth’s topographic surface deformations using projective differential geometry methods as an expression of the space metric tensor and the group of main linear defo...
By the earthquake prediction in areas of earth crust tension on measurements of stations of global navigation systems
Objective. The research objective is to determine relationship between crust tension forces and forces that operate in near-Earth space and earthquakes in entrails of the Earth, based on that was identifying opportunitie...