Dynamics of the North Sea pole tide reconsidered
The anomalous tide in the North Sea, driven by the Chandler wobble, is here re-examined. A previously published solution in which these ‘pole tide’ observations were explained as a forced co-oscillation from the deep water tide is shown to be untenable, because it is very unlikely that the deep ocea...
| Published in: | Geophysical Journal International |
|---|---|
| Main Author: | |
| Format: | Text |
| Language: | English |
| Published: |
Oxford University Press
1986
|
| Subjects: | |
| Online Access: | http://gji.oxfordjournals.org/cgi/content/short/87/3/869 https://doi.org/10.1111/j.1365-246X.1986.tb01974.x |