This contribution deals with the derivation of explicit expressions of the gradients of first, second and third order of the gravitational potential. This is accomplished in the framework of tensor analysis which naturally allows to apply general formulae to the specific coordinate systems in use in geodesy. In particular it is recalled here that when the potential field is expressed in general coordinates on a 3D manifold, the gradient operation leads to the definition of the covariant derivative and that the covariant derivative of a tensor can be obtained by application of a simple rule. When applied to the gravitational potential or to any of its gradients, the rule straightforwardly provides the expressions of the higher-order gradi...
Manifolds, particularly space curves: basic notions 1 The first groundform, the covariant metric t...
General expressions of magnetic vector (MV) and magnetic gradient tensor (MGT) in terms of the first...
The forthcoming GOCE mission will produce gravity gradient data at satellite altitude and consequen...
Based on the Tesseroids software, We offer the codes for modeling the gravitational curvatures of te...
High order, high precision geopotential models have broad application. Computing gravity and gravity...
During the last 20 years, geophysicists have developed great interest in using gravity gradient tens...
Summary. This paper introduces a new matrix computationai approach to the local determination of gra...
International audienceWe present a new analytical solution to compute the full-tensor gravity gradie...
All the elements of the E¨otv¨os tensor can be measured by torsion balance, except the vertical gra...
The relative variation of the vertical gravity gradient on an equipotential ellipsoid is given as a ...
This work is concerned with the comparison of four of the best-known methods for the computation of ...
Abstract In this paper, we propose an inverse method for full gravity gradient tensor data in the sp...
Four widely used algorithms for the computation of the Earth's gravitational potential and its first...
Abstract:When the computational point is approaching the poles, the variance and covariance formulae...
When the computational point is approaching the poles, the variance and covariance formulae of the d...
Manifolds, particularly space curves: basic notions 1 The first groundform, the covariant metric t...
General expressions of magnetic vector (MV) and magnetic gradient tensor (MGT) in terms of the first...
The forthcoming GOCE mission will produce gravity gradient data at satellite altitude and consequen...
Based on the Tesseroids software, We offer the codes for modeling the gravitational curvatures of te...
High order, high precision geopotential models have broad application. Computing gravity and gravity...
During the last 20 years, geophysicists have developed great interest in using gravity gradient tens...
Summary. This paper introduces a new matrix computationai approach to the local determination of gra...
International audienceWe present a new analytical solution to compute the full-tensor gravity gradie...
All the elements of the E¨otv¨os tensor can be measured by torsion balance, except the vertical gra...
The relative variation of the vertical gravity gradient on an equipotential ellipsoid is given as a ...
This work is concerned with the comparison of four of the best-known methods for the computation of ...
Abstract In this paper, we propose an inverse method for full gravity gradient tensor data in the sp...
Four widely used algorithms for the computation of the Earth's gravitational potential and its first...
Abstract:When the computational point is approaching the poles, the variance and covariance formulae...
When the computational point is approaching the poles, the variance and covariance formulae of the d...
Manifolds, particularly space curves: basic notions 1 The first groundform, the covariant metric t...
General expressions of magnetic vector (MV) and magnetic gradient tensor (MGT) in terms of the first...
The forthcoming GOCE mission will produce gravity gradient data at satellite altitude and consequen...