The topographic bias in Stokes’ formula vs. the error of analytical continuation by an Earth Gravitational Model - are they the same?
Geoid determination below the topographic surface in continental areas using analytical continuation of gravity anomaly and/or an external type of solid spherical harmonics determined by an Earth GravitationalModel (EGM) inevitably leads to a topographic bias, as the true disturbing potential at the...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Sciendo
2015-12-01
|
| Series: | Journal of Geodetic Science |
| Subjects: | |
| Online Access: | http://www.degruyter.com/view/j/jogs.2015.5.issue-1/jogs-2015-0017/jogs-2015-0017.xml?format=INT |