Abstract:When the computational point is approaching the poles, the variance and covariance formulae of the disturbing gravity gradient tensors tend to be infinite, and this is a singular problem. In order to solve the problem, the authors deduced the practical non-singular computational formulae of the first-and second-order derivatives of the Legendre functions and two kinds of spherical harmonic functions, and then constructed the nonsingular formulae of variance and covariance function of disturbing gravity gradient tensors
During the last 20 years, geophysicists have developed great interest in using gravity gradient tens...
<p>Slides for the oral presentation "Computation of the gravity gradient tensor due to topographic m...
This work is concerned with the comparison of four of the best-known methods for the computation of ...
When the computational point is approaching the poles, the variance and covariance formulae of the d...
Accurate and highly precise gravity gradient data are an important component of, for example, gravit...
This contribution deals with the derivation of explicit expressions of the gradients of first, seco...
International audienceWe present a new analytical solution to compute the full-tensor gravity gradie...
Representation of data on the sphere is conventionally done using spherical harmonics. Making use of...
High order, high precision geopotential models have broad application. Computing gravity and gravity...
Four widely used algorithms for the computation of the Earth's gravitational potential and its first...
General expressions of magnetic vector (MV) and magnetic gradient tensor (MGT) in terms of the first...
Summary. This paper introduces a new matrix computationai approach to the local determination of gra...
All the elements of the E¨otv¨os tensor can be measured by torsion balance, except the vertical gra...
THE gravity disturbing potential T can be calculated by gravity gradient componentsTij(Txx, Txy, Txz...
The relative variation of the vertical gravity gradient on an equipotential ellipsoid is given as a ...
During the last 20 years, geophysicists have developed great interest in using gravity gradient tens...
<p>Slides for the oral presentation "Computation of the gravity gradient tensor due to topographic m...
This work is concerned with the comparison of four of the best-known methods for the computation of ...
When the computational point is approaching the poles, the variance and covariance formulae of the d...
Accurate and highly precise gravity gradient data are an important component of, for example, gravit...
This contribution deals with the derivation of explicit expressions of the gradients of first, seco...
International audienceWe present a new analytical solution to compute the full-tensor gravity gradie...
Representation of data on the sphere is conventionally done using spherical harmonics. Making use of...
High order, high precision geopotential models have broad application. Computing gravity and gravity...
Four widely used algorithms for the computation of the Earth's gravitational potential and its first...
General expressions of magnetic vector (MV) and magnetic gradient tensor (MGT) in terms of the first...
Summary. This paper introduces a new matrix computationai approach to the local determination of gra...
All the elements of the E¨otv¨os tensor can be measured by torsion balance, except the vertical gra...
THE gravity disturbing potential T can be calculated by gravity gradient componentsTij(Txx, Txy, Txz...
The relative variation of the vertical gravity gradient on an equipotential ellipsoid is given as a ...
During the last 20 years, geophysicists have developed great interest in using gravity gradient tens...
<p>Slides for the oral presentation "Computation of the gravity gradient tensor due to topographic m...
This work is concerned with the comparison of four of the best-known methods for the computation of ...