TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA
P(論文) Tidal currents were observed at the Kita-no-seto Strait near Syowa Station for 15 days from January to February, 1982 by the 23rd Japanese Antarctic Research Expedition. The observed currents show a semidiurnal type in contrast with the tides at Syowa Station showing a mixed type. Judging from...
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Language: | English |
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National Institute of Polar Research
1990
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Online Access: | https://nipr.repo.nii.ac.jp/record/2624/files/KJ00002368236.pdf https://doi.org/10.15094/00002624 https://nipr.repo.nii.ac.jp/records/2624 |
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author | オダマキ, ミノル オオカ, カツジロウ ODAMAKI, Minoru OKA, Katsujiro |
author_facet | オダマキ, ミノル オオカ, カツジロウ ODAMAKI, Minoru OKA, Katsujiro |
author_sort | オダマキ, ミノル |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) Tidal currents were observed at the Kita-no-seto Strait near Syowa Station for 15 days from January to February, 1982 by the 23rd Japanese Antarctic Research Expedition. The observed currents show a semidiurnal type in contrast with the tides at Syowa Station showing a mixed type. Judging from the amplitude and phase lag distributions around Antarctica, M2 tidal wave is understood as a standing wave which has a node near the Station. Therefore, the disagreement of the characteristics is interpreted as that the vertical oscillation (tide) is reduced and the horizontal movement (tidal current) becomes significant around the node. K1 tidal wave is understood as a progressive wave which is trapped to the Antarctic coast and traveling from east to west once a day around Antarctica. This understanding agrees with the fact that the phase lag of K1 tidal current at the Strait is close to that of K1 tide at Syowa Station. departmental bulletin paper |
genre | Antarc* Antarctic Antarctica East Antarctica |
genre_facet | Antarc* Antarctic Antarctica East Antarctica |
geographic | Antarctic The Antarctic East Antarctica Syowa Station Kita-no-seto |
geographic_facet | Antarctic The Antarctic East Antarctica Syowa Station Kita-no-seto |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002624 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(39.583,39.583,-69.000,-69.000) |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00002624 |
op_relation | Proceedings of the NIPR Symposium on Antarctic Geosciences 4 100 107 AA1072335X https://nipr.repo.nii.ac.jp/record/2624/files/KJ00002368236.pdf https://doi.org/10.15094/00002624 https://nipr.repo.nii.ac.jp/records/2624 |
publishDate | 1990 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002624 2025-04-13T14:09:18+00:00 TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA オダマキ, ミノル オオカ, カツジロウ ODAMAKI, Minoru OKA, Katsujiro 1990-09 application/pdf https://nipr.repo.nii.ac.jp/record/2624/files/KJ00002368236.pdf https://doi.org/10.15094/00002624 https://nipr.repo.nii.ac.jp/records/2624 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 4 100 107 AA1072335X https://nipr.repo.nii.ac.jp/record/2624/files/KJ00002368236.pdf https://doi.org/10.15094/00002624 https://nipr.repo.nii.ac.jp/records/2624 1990 ftnipr https://doi.org/10.15094/00002624 2025-03-19T10:19:57Z P(論文) Tidal currents were observed at the Kita-no-seto Strait near Syowa Station for 15 days from January to February, 1982 by the 23rd Japanese Antarctic Research Expedition. The observed currents show a semidiurnal type in contrast with the tides at Syowa Station showing a mixed type. Judging from the amplitude and phase lag distributions around Antarctica, M2 tidal wave is understood as a standing wave which has a node near the Station. Therefore, the disagreement of the characteristics is interpreted as that the vertical oscillation (tide) is reduced and the horizontal movement (tidal current) becomes significant around the node. K1 tidal wave is understood as a progressive wave which is trapped to the Antarctic coast and traveling from east to west once a day around Antarctica. This understanding agrees with the fact that the phase lag of K1 tidal current at the Strait is close to that of K1 tide at Syowa Station. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Antarctica East Antarctica National Institute of Polar Research Repository, Japan Antarctic The Antarctic East Antarctica Syowa Station Kita-no-seto ENVELOPE(39.583,39.583,-69.000,-69.000) |
spellingShingle | オダマキ, ミノル オオカ, カツジロウ ODAMAKI, Minoru OKA, Katsujiro TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA |
title | TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA |
title_full | TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA |
title_fullStr | TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA |
title_full_unstemmed | TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA |
title_short | TIDES AND TIDAL CURRENTS IN THE ANTARCTIC SEA OBSERVED AT SYOWA STATION, EAST ANTARCTICA |
title_sort | tides and tidal currents in the antarctic sea observed at syowa station, east antarctica |
url | https://nipr.repo.nii.ac.jp/record/2624/files/KJ00002368236.pdf https://doi.org/10.15094/00002624 https://nipr.repo.nii.ac.jp/records/2624 |