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温暖化による台風強大化に伴う東京湾での最大級高潮と波浪の時空間分布
https://nied-repo.bosai.go.jp/records/5627
https://nied-repo.bosai.go.jp/records/5627f12acb14-4562-4d6b-b3f1-a2ba9d4740e3
| Item type | researchmap(1) | |||||||||||||||||||||||||||||
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| 公開日 | 2023-03-30 | |||||||||||||||||||||||||||||
| タイトル | ||||||||||||||||||||||||||||||
| 言語 | ja | |||||||||||||||||||||||||||||
| タイトル | 温暖化による台風強大化に伴う東京湾での最大級高潮と波浪の時空間分布 | |||||||||||||||||||||||||||||
| タイトル | ||||||||||||||||||||||||||||||
| 言語 | en | |||||||||||||||||||||||||||||
| タイトル | Distributions of Possible Maximum Storm Surges and High Waves in Tokyo Bay under Global Warming Affected Climate | |||||||||||||||||||||||||||||
| 言語 | ||||||||||||||||||||||||||||||
| 言語 | eng | |||||||||||||||||||||||||||||
| 著者 |
村上 智一
× 村上 智一
× 深尾 宏矩
× 吉野 純
× 安田 孝志
× 飯塚 聡
× 下川 信也
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| 抄録 | ||||||||||||||||||||||||||||||
| 内容記述タイプ | Other | |||||||||||||||||||||||||||||
| 内容記述 | In this study, a climate in September of 2099 based on the SRES A1B scenario was assumed as the future climate affected by the global warming. 50 cases of potential typhoons striking Tokyo Bay under the assumed future climate were estimated by using potential vorticity bogussing scheme of a tropical cyclone. Then, distributions of the possible maximum storm surges and high waves generated by the 50 potential typhoons were predicted by using an atmosphere-ocean-wave coupled model. The results show that the potential storm tide in Tokyo Port reaches 3.4 m and the maximum storm tide of 4.1 m height in Tokyo Bay is caused in Katunan located at the most inner part of Tokyo Bay. The heights of these storm tides remarkably exceed the largest storm tide 2.3 m ever recorded in Tokyo Bay. | |||||||||||||||||||||||||||||
| 言語 | ja | |||||||||||||||||||||||||||||
| 抄録 | ||||||||||||||||||||||||||||||
| 内容記述タイプ | Other | |||||||||||||||||||||||||||||
| 内容記述 | In this study, a climate in September of 2099 based on the SRES A1B scenario was assumed as the future climate affected by the global warming. 50 cases of potential typhoons striking Tokyo Bay under the assumed future climate were estimated by using potential vorticity bogussing scheme of a tropical cyclone. Then, distributions of the possible maximum storm surges and high waves generated by the 50 potential typhoons were predicted by using an atmosphere-ocean-wave coupled model. The results show that the potential storm tide in Tokyo Port reaches 3.4 m and the maximum storm tide of 4.1 m height in Tokyo Bay is caused in Katunan located at the most inner part of Tokyo Bay. The heights of these storm tides remarkably exceed the largest storm tide 2.3 m ever recorded in Tokyo Bay. | |||||||||||||||||||||||||||||
| 言語 | en | |||||||||||||||||||||||||||||
| 書誌情報 |
ja : 土木学会論文集B2(海岸工学) en : Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering) 巻 67, 号 2, p. I_396-I_400, 発行日 2011 |
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| 言語 | ja | |||||||||||||||||||||||||||||
| 出版者 | 公益社団法人 土木学会 | |||||||||||||||||||||||||||||
| 出版者 | ||||||||||||||||||||||||||||||
| 言語 | en | |||||||||||||||||||||||||||||
| 出版者 | Japan Society of Civil Engineers | |||||||||||||||||||||||||||||
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| 収録物識別子タイプ | ISSN | |||||||||||||||||||||||||||||
| 収録物識別子 | 1884-2399 | |||||||||||||||||||||||||||||
| DOI | ||||||||||||||||||||||||||||||
| 関連識別子 | 10.2208/kaigan.67.I_396 | |||||||||||||||||||||||||||||
