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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| Other Authors: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
1976
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| Online Access: | http://hdl.handle.net/2078.1/66669 |
| _version_ | 1821811312689152000 |
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| author | Moens, M. |
| author2 | UCL |
| author_facet | Moens, M. |
| author_sort | Moens, M. |
| collection | DIAL@USL-B (Université Saint-Louis, Bruxelles) |
| description | 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 |
| format | Article in Journal/Newspaper |
| genre | Arctic Longyearbyen Spitsbergen |
| genre_facet | Arctic Longyearbyen Spitsbergen |
| geographic | Arctic Longyearbyen |
| geographic_facet | Arctic Longyearbyen |
| id | ftunistlouisbrus:oai:dial.uclouvain.be:boreal:66669 |
| institution | Open Polar |
| language | English |
| op_collection_id | ftunistlouisbrus |
| op_relation | boreal:66669 http://hdl.handle.net/2078.1/66669 urn:ISSN:0031-9201 |
| op_source | Physics of the Earth and Planetary Interiors, Vol. 13, no. 3, p. 197-211 (1976) |
| publishDate | 1976 |
| record_format | openpolar |
| spelling | ftunistlouisbrus:oai:dial.uclouvain.be:boreal:66669 2025-01-16T20:17:03+00:00 Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) Moens, M. UCL 1976 http://hdl.handle.net/2078.1/66669 eng eng boreal:66669 http://hdl.handle.net/2078.1/66669 urn:ISSN:0031-9201 Physics of the Earth and Planetary Interiors, Vol. 13, no. 3, p. 197-211 (1976) info:eu-repo/semantics/article 1976 ftunistlouisbrus 2024-04-18T18:11:43Z 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 Article in Journal/Newspaper Arctic Longyearbyen Spitsbergen DIAL@USL-B (Université Saint-Louis, Bruxelles) Arctic Longyearbyen |
| spellingShingle | Moens, M. Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) |
| title | Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) |
| title_full | Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) |
| title_fullStr | Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) |
| title_full_unstemmed | Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) |
| title_short | Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) |
| title_sort | solid earth tide and arctic oceanic loading tide at longyearbyen (spitsbergen) |
| url | http://hdl.handle.net/2078.1/66669 |