The geoid is an equipotential surface of the static Earth's gravity field which plays a
fundamental role in definition of physical heights related to the mean sea level (orthometric …

The study proposes a new mathematical method, referred to as spectral combination, to
downscale Gravity Recovery And Climate Experiment (GRACE) observations. The goal is to …

The launch of gravity-dedicated satellite missions at the beginning of the new millennium led
to an accuracy improvement of global Earth gravity field models (GGMs). One of these …

Accurately estimating hydrological parameters is crucial for comprehending global water
resources and climate dynamics. This study addresses the challenge of quantifying …

The invariants of gravity (or gravitational) gradient tensor can be applied as the additional
internal parameters for the gravity gradient tensor, which have been widely used in the …

In recent years, there are research trends from constant to variable density and low-order to
high-order gravitational potential gradients in gravity field modeling. Under the research …

In geophysical and geodetic studies, gravity inversion is typically performed such that
observed gravity values are first continued downward onto a regular (planar, spherical or …

Previous studies mainly focused on second-and third-order gravitational potential gradients
that these values are already measurable or that appropriate measurement principles are …

Second-and third-order gravitational potential derivatives can be employed for the
determination of the medium-and high-frequency parts of the Earth's gravity field. Due to the …

In this study, we apply a spectral combination method for estimation of height anomalies
from gradients of the gravitational potential measured by satellites. The spectral combination …