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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Main Authors: オダマキ, ミノル, オオカ, カツジロウ, ODAMAKI, Minoru, OKA, Katsujiro
Language:English
Published: National Institute of Polar Research 1990
Subjects:
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