The recovery of local (time-variable) gravity features from satellite-to-satellite tracking missions is one of the current challenges in Geodesy. Often, a global spherical harmonic analysis is used and the area of interest is selected later on. However, this approach has deficiencies since leakage and incomplete recovery of signal are common side effects. In order to make better use of the signal content, a gravity recovery using localizing base functions can be employed. In this paper, two different techniques are compared in a case study using simulated potential observations at satellite level – namely position-optimized radial base functions and a single layer representation using a piecewise continuous density. The first one is the mor...
The geoid is an equipotential surface of Earth's gravity field, coinciding with mean ocean surface l...
In this study we address the question of whether regional gravity field modeling techniques of GRACE...
textAs an alternative to spherical harmonics in modeling the gravity field of the Earth, we built a ...
The recovery of local (time-variable) gravity features from satellite-to-satellite tracking missions...
The choice of the optimal spherical radial basis function (SRBF) in local gravity field modelling fr...
The choice of the optimal spherical radial basis function (SRBF) in local gravity field modelling fr...
In this thesis, an integrated approach is developed for the regional refinement of global gravity fi...
peer reviewedGlobal gravity solutions are generally influenced by degenerating effects such as insuf...
Gravity fields are mainly represented in spherical har-monics, which causes problems in the regional...
We propose a methodology for local gravity field modelling from gravity data using spherical radial ...
The gravity field is a signature of the mass distribution and interior structure of the Earth, in ad...
The paper is about a methodology to combine a noisy satellite-only global gravity field model (GGM) ...
The inverse problem of recovering the Earth's density distribution from data of the first or second ...
This study presents a solution of the ‘1 cm Geoid Experiment’ (Colorado Experiment) using spherical ...
The purpose of GPS-satellite-to-satellite tracking (GPS-SST) is to determine the gravitational poten...
The geoid is an equipotential surface of Earth's gravity field, coinciding with mean ocean surface l...
In this study we address the question of whether regional gravity field modeling techniques of GRACE...
textAs an alternative to spherical harmonics in modeling the gravity field of the Earth, we built a ...
The recovery of local (time-variable) gravity features from satellite-to-satellite tracking missions...
The choice of the optimal spherical radial basis function (SRBF) in local gravity field modelling fr...
The choice of the optimal spherical radial basis function (SRBF) in local gravity field modelling fr...
In this thesis, an integrated approach is developed for the regional refinement of global gravity fi...
peer reviewedGlobal gravity solutions are generally influenced by degenerating effects such as insuf...
Gravity fields are mainly represented in spherical har-monics, which causes problems in the regional...
We propose a methodology for local gravity field modelling from gravity data using spherical radial ...
The gravity field is a signature of the mass distribution and interior structure of the Earth, in ad...
The paper is about a methodology to combine a noisy satellite-only global gravity field model (GGM) ...
The inverse problem of recovering the Earth's density distribution from data of the first or second ...
This study presents a solution of the ‘1 cm Geoid Experiment’ (Colorado Experiment) using spherical ...
The purpose of GPS-satellite-to-satellite tracking (GPS-SST) is to determine the gravitational poten...
The geoid is an equipotential surface of Earth's gravity field, coinciding with mean ocean surface l...
In this study we address the question of whether regional gravity field modeling techniques of GRACE...
textAs an alternative to spherical harmonics in modeling the gravity field of the Earth, we built a ...