Temporal Variations of the Geopotential Atmospheric Excitation
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Engineering topics
Publications and source records attributed to Dong, D..
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Seasonal variations in the Earth's gravitational field are investigated through the analyis of LAGEOS I satellite laser ranging measurements and are compared with those produced by atmospheric mass redistribution as inferred from global surface pressure date from the National Centers for Environmental Prediction (NCEP) reanalyses.
We discuss an approach for efficiently combining different types of geodetic data to estimate time-dependent motions of stations in a region of active deformation.
The geocenter variations reflect the global scale mass redistribution and the interaction between the solid Earth and the mass load.
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Seasonal variations in the Earth's gravitational field are investigated through the analysis of LAGEOS I satellite laser ranging measurements spanning 1984 to 1992. Global surface pressure data are analyzed; a self-consistent equilibrium ocean tide model is used to compute the effect of the gravitational field on tides. Laser ranging measurements are used to model gravitational field effects.
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Thirteen years of satellite laser ranging measurements to LAGEOS (1980-1992) have been analyzed to investigate the variations of the Earth's gravity field.
Laser ranging measurements to single satellite are sensitive to the Earth's gravitational field and its temporal variations. Using 13 years (1980-1992) of LAGEOS I laser ranging data, we have recovered monthly mean linear combinations of even and odd degree zonal spherical harmonic coefficients of the Earth's gravitational field.
Besides operating its own energy budget, an earthquake acts as an agent transferring a much greater amount of energy among the Earth's rotation, elastic field, gravitational field, and internal heat.