We present the latest 3D velocity field of the Fennoscandian glacial isostatic adjustment
(GIA) process from BIFROST. It is derived from more than 4800 days (13 years) of data at …

The least squares modification of Stokes' formula reduces the impact of the errors stemming
from truncation, erroneous terrestrial gravity data and potential harmonics in a least squares …

Today the combination of Stokes' formula and an Earth gravity model (EGM) for geoid
determination is a standard procedure. However, the method of modifying Stokes' formula …

In a modern application of Stokes' formula for geoid determination, regional terrestrial gravity
is combined with long-wavelength gravity information supplied by an Earth gravity model …

Abstract Global Navigation Satellite System positioning of gravity surveys permits geoid
computation via Hotine's integral. A suite of modifications is presented so that the user can …

Sudan is characterized by vast area with flat terrains in most of the country's regions and
therefore the existence of a high-resolution geoid model is considered very important …

An argument is put forward in favor of using a model gravity field of a degree and order
higher than 2 as a reference in gravity field studies. Stokes's approach to the evaluation of …

Computational stages of a new high-resolution 5 mm quasigeoid model for Estonia are
explained. Certain requirements for the quality and coverage of gravity data in the context of …

To calibrate airborne gravity gradiometers currently in development in China, it is urgent to
build an airborne gravity gradiometer test site. The site's selection depends on the …

Since 2006, several different groups have computed geoid and/or quasigeoid (quasi/geoid)
models for the Auvergne test area in central France using various approaches. In this …