The gravity and shape data acquired by the Dawn spacecraft during its primary mission
revealed that Ceres is partially differentiated with an interior structure consistent with a …

We analyse spatial and spectral characteristics of various refined gravity data used for
modelling and gravimetric interpretation of the crust–mantle interface and the mantle …

Filtering is a necessary step in the Gravity Recovery and Climate Experiment (GRACE) data
processing, but leads to signal leakage and attenuation obviously, and adversely affects the …

Most studies on gravity forward modeling in the spectral domain truncate the gravitational
potential spectra at a resolution commensurate with the input topographic mass model. This …

The realization over the last decade of dedicated gravity field satellite missions enabled the
production of a series of new satellite‐only and combined models for the Earth's gravity field …

We developed and applied a novel numerical scheme for a gravimetric forward modelling of
the Earth's crustal density structures based entirely on methods for a spherical analysis and …

Forward gravity modeling in the spectral domain traditionally relies on spherical
approximation. However, this level of approximation is insufficient for some present day high …

A long-wavelength geoidal geometry characterizes the most pronounced features of the
Indian Ocean geoid low and the West Pacific and North Atlantic geoid highs. These large …

Different interpretations of crustal thickness variations have been proposed for central
Mexico. The studied region encompass the transition between the Mesa Central, an …

Mass associated with surface topography makes a significant contribution to the Earth's
gravitational potential at all spectral scales. Accurate computation in spherical harmonics to …