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 …

The ocean's mean dynamic topography (MDT) is the surface representation of ocean
circulation. It may be determined by the ocean approach, using numerical ocean circulation …

The deduction of a regularly spaced gravity anomaly grid from scattered survey data is
studied, addressing mainly two aspects: reduction of gravity to anomalies and subsequent …

Geoid and quasigeoid modelling from gravity anomalies by the method of least squares
modification of Stokes's formula with additive corrections is adapted for the usage with …

In the context of a GOCE regional validation and combination experiment in Germany, a
work package within the framework of the GOCE-GRAND II project, gravity observations …

We consider the problem of local (quasi-) geoid modelling from terrestrial gravity anomalies.
Whereas this problem is uniquely solvable (up to spherical harmonic degree one) if gravity …

Due to increasing accuracy in measurements of the earth's gravity potential from
satellitemissions the goeid can be computed with higher resolution and accuracy than …

Due to the challenge that the Amazon Basin imposes for traditional geodetic surveys, the
Brazilian Fundamental Vertical Network (BFVN) is materialized in two independent parts: the …

The aim of the paper is to show a methodology in order to build a local geoid model using
the Compute-Remove-Restore technique; to achieve this aim, suitable algorithms in …

In this paper an overdetermined Geodetic Boundary Value Problem (GBVP) approach for
telluroid and quasi-geoid computations is presented. The presented GBVP approach can …