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 …

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 …

A deterministic modification of Stokes's integration kernel is presented which reduces the
truncation error when regional gravity data are used in conjunction with a global …

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 …

When regional gravity data are used to compute a gravimetric geoid in conjunction with a
geopotential model, it is sometimes implied that the terrestrial gravity data correct any …

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 …

Any errors in digital elevation models (DEMs) will introduce errors directly in gravity
anomalies and geoid models when used in interpolating Bouguer gravity anomalies. Errors …