Using models of the ocean's mean dynamic topography to identify errors in coastal geodetic levelling
Identifying errors (blunders and systematic errors) in coastal geodetic levelling networks has often been problematic. This is because (1) mean sea level (MSL) at tide gauges cannot be directly compared to height differences from levelling because the geoid/quasigeoid and MSL are not parallel, being...
| Main Author: | |
|---|---|
| Format: | Journal Article |
| Published: |
Taylor and Francis
2014
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/6117 |