Add to ORKGNew integral formulas to determine geopotential coefficients from terrestrial gravity and satellite altimetry data are given. The formulas are based on the integration of data over the non-spherical surface of the Earth. The effect of the topography to low degrees and orders of coefficients is estimated numerically. Formulas for the solution of the gravimetric boundary value problem are derived
Before the computation of short-wavelength and long-wavelength components of the geoid undulations f...
In solution of gradiometric boundary value problem in space a regular grid of satellite gravity grad...
A method to accurately determine certain constants appearing in mathematical representations of the ...
Integral formulas in the parameter domain are used instead of a representation by spherical harmonic...
Different forms of the theoretical gravity formula are summarized and methods of standardization of ...
For the determination of geopotential coefficients, data can be used from rather different sources, ...
The formulas for the determination of the coefficients of the spherical harmonic expansion of the di...
Linear estimation theory, along with a new technique to compute relative data weights, was applied t...
The determination of the Earth's gravitational potential can be done through the analysis of satelli...
One of the most important stages in the computation of a global geopotential model is the computatio...
Knowledge of the earth's gravity field continued to increase during the last four years. Altimetry d...
A new, geometrical, first order, nonresonant, frozen orbit theory was developed based on Orlov's uni...
On the assumption that the compensation for the topographic load is achieved in the manner of Airy-H...
A numerical method for the determination of gravity anomalies from geoid heights is described using ...
Laser data from nine satellites and 12 stations are combined with surface-gravity data to obtain sph...
Before the computation of short-wavelength and long-wavelength components of the geoid undulations f...
In solution of gradiometric boundary value problem in space a regular grid of satellite gravity grad...
A method to accurately determine certain constants appearing in mathematical representations of the ...
Integral formulas in the parameter domain are used instead of a representation by spherical harmonic...
Different forms of the theoretical gravity formula are summarized and methods of standardization of ...
For the determination of geopotential coefficients, data can be used from rather different sources, ...
The formulas for the determination of the coefficients of the spherical harmonic expansion of the di...
Linear estimation theory, along with a new technique to compute relative data weights, was applied t...
The determination of the Earth's gravitational potential can be done through the analysis of satelli...
One of the most important stages in the computation of a global geopotential model is the computatio...
Knowledge of the earth's gravity field continued to increase during the last four years. Altimetry d...
A new, geometrical, first order, nonresonant, frozen orbit theory was developed based on Orlov's uni...
On the assumption that the compensation for the topographic load is achieved in the manner of Airy-H...
A numerical method for the determination of gravity anomalies from geoid heights is described using ...
Laser data from nine satellites and 12 stations are combined with surface-gravity data to obtain sph...
Before the computation of short-wavelength and long-wavelength components of the geoid undulations f...
In solution of gradiometric boundary value problem in space a regular grid of satellite gravity grad...
A method to accurately determine certain constants appearing in mathematical representations of the ...