To reduce the numerical complexity of inverse solutions to large systems of discretised integral equations in gravimetric geoid/quasigeoid modelling, the surface domain of Green’s integrals is subdivided into the near-zone and far-zone integration sub-domains. The inversion is performed for the near zone using regional detailed gravity data. The far-zone contributions to the gravity field quantities are estimated from an available global geopotential model using techniques for a spherical harmonic analysis of the gravity field. For computing the far-zone contributions by means of Green’s integrals, truncation coefficients are applied. Different forms of truncation coefficients have been derived depending on a type of integrals in solving va...
There are numerous methods to modify Stokes’ formula with the usually common feature of reducing the...
Global models of the Earth gravity field and topographic/bathymetric data can be used for the gravim...
The isostatic gravity anomalies have been traditionally used to solve the inverse problems of isosta...
To reduce the numerical complexity of inverse solutions to large systems of discretised integral equ...
Integral transformations are a useful mathematical apparatus for modelling the gravitational field a...
Spectral gravity forward modelling is a technique that converts a band-limited topography into its i...
AbstractAirborne gravimetry has become a vital technique in local gravity field approximation, and u...
We evaluate the new regional quasigeoid model (OTG12) for New Zealand using the method which utilise...
Airborne gravimetry has become a vital technique in local gravity field approximation, and upward/do...
Determination of the gravimetric geoid is based on inversion of observed values of gravity into the ...
According to Stokes’ approach, given the gravity anomaly on the geoid as the boundary, a disturbing ...
One of the most important stages in the computation of a global geopotential model is the computatio...
Abstract. The purpose of this paper is to further develop a method of combining terrestrial and sat-...
Molodensky G terms are used in the computation of the quasigeoid. We derive error propagation formul...
In geodesy, the geoid and the quasigeoid are used as a reference surface for heights. Despite some s...
There are numerous methods to modify Stokes’ formula with the usually common feature of reducing the...
Global models of the Earth gravity field and topographic/bathymetric data can be used for the gravim...
The isostatic gravity anomalies have been traditionally used to solve the inverse problems of isosta...
To reduce the numerical complexity of inverse solutions to large systems of discretised integral equ...
Integral transformations are a useful mathematical apparatus for modelling the gravitational field a...
Spectral gravity forward modelling is a technique that converts a band-limited topography into its i...
AbstractAirborne gravimetry has become a vital technique in local gravity field approximation, and u...
We evaluate the new regional quasigeoid model (OTG12) for New Zealand using the method which utilise...
Airborne gravimetry has become a vital technique in local gravity field approximation, and upward/do...
Determination of the gravimetric geoid is based on inversion of observed values of gravity into the ...
According to Stokes’ approach, given the gravity anomaly on the geoid as the boundary, a disturbing ...
One of the most important stages in the computation of a global geopotential model is the computatio...
Abstract. The purpose of this paper is to further develop a method of combining terrestrial and sat-...
Molodensky G terms are used in the computation of the quasigeoid. We derive error propagation formul...
In geodesy, the geoid and the quasigeoid are used as a reference surface for heights. Despite some s...
There are numerous methods to modify Stokes’ formula with the usually common feature of reducing the...
Global models of the Earth gravity field and topographic/bathymetric data can be used for the gravim...
The isostatic gravity anomalies have been traditionally used to solve the inverse problems of isosta...