North Atlantic Ocean: Preliminary Description of Normal Modes
The three lowest gravitational modes of free oscillation of the North Atlantic Ocean are estimated by numerical integration of Laplace's tidal equations. These modes have periods of approximately 21, 14, and 11 hours, and structures, respectively, of one, two, and three positive amphidromic sys...
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American Association for the Advancement of Science (AAAS)
1972
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craaas:10.1126/science.178.4057.156 2024-06-09T07:48:00+00:00 North Atlantic Ocean: Preliminary Description of Normal Modes Platzman, George W. 1972 http://dx.doi.org/10.1126/science.178.4057.156 https://www.science.org/doi/pdf/10.1126/science.178.4057.156 en eng American Association for the Advancement of Science (AAAS) Science volume 178, issue 4057, page 156-157 ISSN 0036-8075 1095-9203 journal-article 1972 craaas https://doi.org/10.1126/science.178.4057.156 2024-05-16T12:54:05Z The three lowest gravitational modes of free oscillation of the North Atlantic Ocean are estimated by numerical integration of Laplace's tidal equations. These modes have periods of approximately 21, 14, and 11 hours, and structures, respectively, of one, two, and three positive amphidromic systems. The phase distribution of the first mode resembles cotidal charts of the diurnal tide, and the period of the second mode is consistent with that inferred by Wunsch from tidal data in Bermuda and the Azores. Article in Journal/Newspaper North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 178 4057 156 157 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
The three lowest gravitational modes of free oscillation of the North Atlantic Ocean are estimated by numerical integration of Laplace's tidal equations. These modes have periods of approximately 21, 14, and 11 hours, and structures, respectively, of one, two, and three positive amphidromic systems. The phase distribution of the first mode resembles cotidal charts of the diurnal tide, and the period of the second mode is consistent with that inferred by Wunsch from tidal data in Bermuda and the Azores. |
format |
Article in Journal/Newspaper |
author |
Platzman, George W. |
spellingShingle |
Platzman, George W. North Atlantic Ocean: Preliminary Description of Normal Modes |
author_facet |
Platzman, George W. |
author_sort |
Platzman, George W. |
title |
North Atlantic Ocean: Preliminary Description of Normal Modes |
title_short |
North Atlantic Ocean: Preliminary Description of Normal Modes |
title_full |
North Atlantic Ocean: Preliminary Description of Normal Modes |
title_fullStr |
North Atlantic Ocean: Preliminary Description of Normal Modes |
title_full_unstemmed |
North Atlantic Ocean: Preliminary Description of Normal Modes |
title_sort |
north atlantic ocean: preliminary description of normal modes |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1972 |
url |
http://dx.doi.org/10.1126/science.178.4057.156 https://www.science.org/doi/pdf/10.1126/science.178.4057.156 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Science volume 178, issue 4057, page 156-157 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.178.4057.156 |
container_title |
Science |
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178 |
container_issue |
4057 |
container_start_page |
156 |
op_container_end_page |
157 |
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1801379533389037568 |