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 |
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:66669 |
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:66669 2024-05-12T07:58:55+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 |
| institution |
Open Polar |
| collection |
DIAL@USL-B (Université Saint-Louis, Bruxelles) |
| op_collection_id |
ftunistlouisbrus |
| language |
English |
| 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 |
| author2 |
UCL |
| format |
Article in Journal/Newspaper |
| author |
Moens, M. |
| spellingShingle |
Moens, M. Solid Earth tide and Arctic oceanic loading tide at Longyearbyen (Spitsbergen) |
| author_facet |
Moens, M. |
| author_sort |
Moens, M. |
| title |
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_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_sort |
solid earth tide and arctic oceanic loading tide at longyearbyen (spitsbergen) |
| publishDate |
1976 |
| url |
http://hdl.handle.net/2078.1/66669 |
| geographic |
Arctic Longyearbyen |
| geographic_facet |
Arctic Longyearbyen |
| genre |
Arctic Longyearbyen Spitsbergen |
| genre_facet |
Arctic Longyearbyen Spitsbergen |
| op_source |
Physics of the Earth and Planetary Interiors, Vol. 13, no. 3, p. 197-211 (1976) |
| op_relation |
boreal:66669 http://hdl.handle.net/2078.1/66669 urn:ISSN:0031-9201 |
| _version_ |
1798839551083413504 |