The global marine gravity anomaly model is predominantly recovered from along-track radar
altimeter data. Despite significant advances in gravity anomaly recovery, the improvement of …

The harmonic correction (HC) is one of the key quantities when using residual terrain
modelling (RTM) for high-frequency gravity field modelling. In the RTM technique, high …

The Colorado geoid experiment was initiated and organized as a joint study by the Joint
Working Group (JWG) 2.2. 2 (1-cm geoid experiment) of the International Association of …

The “non-harmonicity” problem in residual terrain modelling (RTM) is a challenging issue,
causing errors exceeding 200 mGal in the RTM gravity anomaly in rugged areas. Although …

Gravity on Earth is of great interest in geodesy, geophysics, and natural resource
exploration. Ship-based gravimeters are a widely used instrument for the collection of …

The deflection of the vertical is one of the essential products of altimetry. However, unlike
gravity and vertical gravity gradients, it is seldom used in bathymetry inversion. In this study …

The development of the global geopotential model (GGM) broadens its applications in
ocean science, which emphasizes the importance for model assessment. We assess the …

We study the role of airborne gravimetry for seamless bathymetry modeling over the Paracel
Islands in the northern South China Sea (SCS) and investigate the possibility of using Ice …

The determination of high‐quality mean dynamic topography (MDT) over island areas faces
multiple challenges, due to the error in a global geopotential model (GGM) as well as the …

The marine gravity field recovery close to land/island is challenging owing to the scarcity of
measured gravimetric observations and sorely contaminated satellite radar altimeter-derived …