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I. Ya. Tsurkis M. S. Kuchay E. A. Spiridonov 《Izvestiya Physics of the Solid Earth》2012,48(4):339-353
The data series of the International Earth Rotation and Reference Systems Service and National Centers for Environmental Prediction
() for 1982–2003 are analyzed. It is shown that the atmospheric component of polar motion can be treated as the anisotropic
Markov process with discrete time, and the torque exerted by the atmosphere on the solid Earth, as the white noise. The intensity
and characteristic correlation time of the process are estimated. The efficiency of the atmospheric mechanism in the excitation
of the Chandler wobble is estimated in the context of the probabilistic model. 相似文献
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Izvestiya, Atmospheric and Oceanic Physics - For regional earthquakes, the kinematic parameter VP/VS, an analog of the TAU parameter, was analyzed in order to study the state of magmatic matter,... 相似文献
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