Digital terrain models are the basis for geodetic, geophysical, oceanograph
ic and other studies in regional or global scale. In gravity field modellin
g the global DTMs ETOPO5, TerrainBase and JGP95E have been used among other
in combination with other data related to the gravity field, for the devel
opment of geopotential models. An intercomparison of these DTMs showed cons
iderable differences between them. The standard deviation of these differen
ces are of the order of 100m, while the minimum and the maximum differences
range from -3.8km to 4.7km were observed. This statistics shows that the m
odels are affected by considerable errors, The refinement of the DTMs will
contribute to the improvement of the gravity field approximation. (C) 2000
Elsevier Science Ltd. All rights reserved.