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...
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| Format: | Other/Unknown Material |
| Language: | unknown |
| Published: |
1986
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| Online Access: | http://ntrs.nasa.gov/search.jsp?R=19870042208 |