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 …

We present a revised estimate of the maximum depth of the Challenger Deep, generally
considered the deepest area of the world's oceans, based on a series of submersible dives …

Downward continuation is a very useful technique in the interpretation of potential field data.
It would enhance the short wavelength of the gravity anomalies or accentuate the details of …

Downward continuation can enhance small‐scale sources and improve resolution.
Nevertheless, the common methods have disadvantages in obtaining optimal results …

Within the modelling of gravity data, a common practice is the upward/downward
continuation of the signal, ie the process of continuing the gravitational signal in the vertical …

Radial basis functions (RBFs) have been used extensively in satellite geodetic applications.
However, to the author's knowledge, their role in processing and modeling airborne gravity …

One of the main applications of the gravity field and steady-state Ocean Circulation Explorer
(GOCE) satellite data is their combination with local gravity anomalies for geoid and gravity …

The truncation coefficient is widely utilized in non-global coverage computations of
geophysics and geodesy and is always altitude dependent. As the two commonly used …

In this paper, a new method for regionally improving global geopotential models (GGMs)
with global navigation satellite system (GNSS)/levelling data is proposed. In this method, the …

The differences between local and reference geopotential values are the fundamental
quantities of interest in the geodetic boundary value problem approach for connecting …