It is well known that periodical and cyclical movements of cosmic sources of gravitation considerably affect Earth’s geospheres (atmosphere, hydrosphere, crust, etc.) by producing tides and related phenomena, as well as the state of tectonic blocks, lithosphere plates and deep crust fractures. The result of such influence may be earthquakes and other catastrophes. Nowadays, the question modeling of geophysical processes is considerably actual. Thus studies in area of Earth’ sciences have been moved from practice of observation of separate phenomena to the systematic quantitative investigation in interdisciplinary areas. A system of two modules is proposed by the author each using its own system of coordinates: (1) the model of three‐dimensional spherical body of the Earth with the system of coordinates (III) including the time of events that happened on the Earth and (2) a compact model of the relative motion of celestial bodies in space and time as vectors that are changing their directions. Note the data bases of the Earth sciences have been used to construct the module (1), while the module (2) has been built using astronomic parameters of celestial bodies. The module (2) is known as “Method of moving source” (MDS) [1, 2]. As a result, on the basis of systematization, joint analysis and complexity of cosmic data and databases of Earth sciences the cause‐and‐effect relations between events on Earth and space bodies are established.
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22 September 2011
NUMERICAL ANALYSIS AND APPLIED MATHEMATICS ICNAAM 2011: International Conference on Numerical Analysis and Applied Mathematics
19–25 September 2011
Halkidiki, (Greece)
Research Article|
September 22 2011
Spatio‐Temporal Modeling of the Earth Events and Moving of Celestial Bodies
Natalia P. Bulatova
Natalia P. Bulatova
Schmidt Institute of Physics of the Earth of Russian Academy of Sciences, Moscow
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AIP Conf. Proc. 1389, 1007–1010 (2011)
Citation
Natalia P. Bulatova; Spatio‐Temporal Modeling of the Earth Events and Moving of Celestial Bodies. AIP Conf. Proc. 22 September 2011; 1389 (1): 1007–1010. https://doi.org/10.1063/1.3637780
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