地球潮汐への海洋潮汐の影響に関する一考察
The Arctic Ocean, Sea of Okhotsk, Yellow Sea, East China Sea and the western half of SetoNaikai do not exert significant influences on the earth tides in Kyoto compared with the PacificOcean, judging from their location and size. The effects of ocean tides in seas farther than adistance of 4000 or 1...
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京都大学防災研究所
1978
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ftkyotouniv:oai:repository.kulib.kyoto-u.ac.jp:2433/70196 2023-05-15T15:00:30+02:00 地球潮汐への海洋潮汐の影響に関する一考察 A COMMENT UPON THE EFFECT OF OCEAN TIDES ON EARTH TIDES 田中, 寅夫 TANAKA, Torao 1978-04-01 application/pdf http://hdl.handle.net/2433/70196 jpn jpn 京都大学防災研究所 Disaster Prevention Research Institute, Kyoto University http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html 0386-412X http://hdl.handle.net/2433/70196 AN00027784 京都大学防災研究所年報. B 21 B-1 137 143 Disaster Prevention Research Institute Annuals. B 448.6 452.6 departmental bulletin paper 1978 ftkyotouniv 2022-01-21T00:17:26Z The Arctic Ocean, Sea of Okhotsk, Yellow Sea, East China Sea and the western half of SetoNaikai do not exert significant influences on the earth tides in Kyoto compared with the PacificOcean, judging from their location and size. The effects of ocean tides in seas farther than adistance of 4000 or 1000 km from Kyoto are concluded to be negligible in cases of tilt or strain tide, respectively, while more distant oceans must be taken into consideration in the case of gravity tidein Kyoto. The effect of the M2 ocean tide on the gravity tide in Kyushu is larger than that inHokkaido due to dominant effects of the northwestern part of the Pacific Ocean and the EastChina Sea in Kyushu; the effect of the Sea of Japan is unexpectedly small. The Arctic Ocean, Sea of Okhotsk, Yellow Sea, East China Sea and the western half of SetoNaikai do not exert significant influences on the earth tides in Kyoto compared with the PacificOcean, judging from their location and size. The effects of ocean tides in seas farther than adistance of 4000 or 1000 km from Kyoto are concluded to be negligible in cases of tilt or strain tide,respectively, while more distant oceans must be taken into consideration in the case of gravity tidein Kyoto. The effect of the M2 ocean tide on the gravity tide in Kyushu is larger than that inHokkaido due to dominant effects of the northwestern part of the Pacific Ocean and the EastChina Sea in Kyushu; the effect of the Sea of Japan is unexpectedly small. Report Arctic Arctic Ocean Kyoto University Research Information Repository (KURENAI) Arctic Arctic Ocean Okhotsk Pacific |
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Open Polar |
collection |
Kyoto University Research Information Repository (KURENAI) |
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ftkyotouniv |
language |
Japanese |
topic |
448.6 452.6 |
spellingShingle |
448.6 452.6 田中, 寅夫 地球潮汐への海洋潮汐の影響に関する一考察 |
topic_facet |
448.6 452.6 |
description |
The Arctic Ocean, Sea of Okhotsk, Yellow Sea, East China Sea and the western half of SetoNaikai do not exert significant influences on the earth tides in Kyoto compared with the PacificOcean, judging from their location and size. The effects of ocean tides in seas farther than adistance of 4000 or 1000 km from Kyoto are concluded to be negligible in cases of tilt or strain tide, respectively, while more distant oceans must be taken into consideration in the case of gravity tidein Kyoto. The effect of the M2 ocean tide on the gravity tide in Kyushu is larger than that inHokkaido due to dominant effects of the northwestern part of the Pacific Ocean and the EastChina Sea in Kyushu; the effect of the Sea of Japan is unexpectedly small. The Arctic Ocean, Sea of Okhotsk, Yellow Sea, East China Sea and the western half of SetoNaikai do not exert significant influences on the earth tides in Kyoto compared with the PacificOcean, judging from their location and size. The effects of ocean tides in seas farther than adistance of 4000 or 1000 km from Kyoto are concluded to be negligible in cases of tilt or strain tide,respectively, while more distant oceans must be taken into consideration in the case of gravity tidein Kyoto. The effect of the M2 ocean tide on the gravity tide in Kyushu is larger than that inHokkaido due to dominant effects of the northwestern part of the Pacific Ocean and the EastChina Sea in Kyushu; the effect of the Sea of Japan is unexpectedly small. |
author2 |
TANAKA, Torao |
format |
Report |
author |
田中, 寅夫 |
author_facet |
田中, 寅夫 |
author_sort |
田中, 寅夫 |
title |
地球潮汐への海洋潮汐の影響に関する一考察 |
title_short |
地球潮汐への海洋潮汐の影響に関する一考察 |
title_full |
地球潮汐への海洋潮汐の影響に関する一考察 |
title_fullStr |
地球潮汐への海洋潮汐の影響に関する一考察 |
title_full_unstemmed |
地球潮汐への海洋潮汐の影響に関する一考察 |
title_sort |
地球潮汐への海洋潮汐の影響に関する一考察 |
publisher |
京都大学防災研究所 |
publishDate |
1978 |
url |
http://hdl.handle.net/2433/70196 |
geographic |
Arctic Arctic Ocean Okhotsk Pacific |
geographic_facet |
Arctic Arctic Ocean Okhotsk Pacific |
genre |
Arctic Arctic Ocean |
genre_facet |
Arctic Arctic Ocean |
op_relation |
http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html 0386-412X http://hdl.handle.net/2433/70196 AN00027784 京都大学防災研究所年報. B 21 B-1 137 143 Disaster Prevention Research Institute Annuals. B |
_version_ |
1766332599585734656 |