Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen)
The three components of the indirect ocean effect are calculated for the M/sub 2/, K/sub 1/ and O/sub 1/ waves and compared with the observed Earth tide. The vertical component of the near Arctic oceanic load explains fairly well the large 45 degrees observed phase lag of M/sub 2/. The results for t...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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1976
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| Online Access: | http://hdl.handle.net/2078.1/66669 |
| Summary: | The three components of the indirect ocean effect are calculated for the M/sub 2/, K/sub 1/ and O/sub 1/ waves and compared with the observed Earth tide. The vertical component of the near Arctic oceanic load explains fairly well the large 45 degrees observed phase lag of M/sub 2/. The results for the horizontal components are satisfactory; the discrepancies between different tiltmeters are not due to the oceanic perturbations (unless some local or cavity effects are supposed). Anglais |
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