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UT Repository >
131 地震研究所 >
東京大学地震研究所彙報 >
Please use this identifier to cite or link to this item:
http://hdl.handle.net/2261/51526
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| タイトル: | 2011年東北地方太平洋沖地震の津波高調査 |
| その他のタイトル: | Field Surveys of Tsunami Heights from the 2011 off the Pacific Coast of Tohoku, Japan Earthquake |
| 著者: | 都司, 嘉宣 佐竹, 健治 石辺, 岳男 楠本, 聡 原田, 智也 西山, 昭仁 金, 幸隆 上野, 俊洋 室谷, 智子 大木, 聖子 杉本, めぐみ 泊, 次郎 Heidarzadeh, Mohammad 綿田, 辰吾 今井, 健太郎 Choi, Byung Ho Yoon, Sung Bum Bae, Jae Seok Kim, Kyeong Ok Kim, Hyun Woo |
| 著者(別言語): | Tsuji, Yoshinobu Satake, Kenji Ishibe, Takeo Kusumoto, Satoshi Harada, Tomoya Nishiyama, Akihito Kim, Haeng Yoong Ueno, Toshihiro Murotani, Satoko Oki, Satoko Sugimoto, Megumi Tomari, Jiro Watada, Shingo Imai, Kentaro |
| キーワード: | the 2011 off the Pacific coast of Tohoku Earthquake tsunami height field survey inundation height runup height tsunami height in port |
| Issue Date: | 16-Mar-2012 |
| 出版者: | 東京大学地震研究所 |
| 掲載誌情報: | 東京大学地震研究所彙報. 第86号第3/4冊, 2012.3.16, pp. 29-279 |
| 抄録: | We report the results of field surveys conducted by the Earthquake Research Institute, to measure tsunami heights from the 2011 off the Pacific coast of Tohoku, Japan Earthquake (M 9.0), on March 11. Measurements were taken at 296 points on the Sanriku coasts of Aomori, Iwate, and Miyagi Prefectures, and the Pacific coasts of Ibaraki and Chiba Prefectures. The data are included in the results of the 2011 Tohoku Earthquake Tsunami Joint Survey Group. We did not cover the Sendai plain in the southern Miyagi Prefecture because other parties extensively measure there, nor Fukushima Prefecture because of the accident of the Fukushima Dai-ichi nuclear power plant. The twelve surveys first sought traces indicating tsunami runup or inundation heights. Reliability was classified into A (most reliable based on clear physical evidence and eyewitness accounts), B (mostly based on natural traces), and C (least reliable based on equivocal evidence). Most physical evidence obtained after June was not significant; therefore, reliance was mostly placed on eyewitness accounts. Locations and relative heights above sea level were measured using handheld GPS receivers, auto-level, or total station. The measured heights were corrected for differences in tide level between measurement time and tsunami arrival time. The results are shown on table and four regional maps; however, the details of each measurement, including locations shown on 1:25,000 maps and photographs of evidence are shown in the Appendix. Along the northern Sanriku coast (Aomori and Iwate), most of the 141 heights range between 10m and 30m. Runup heights exceeding 30m were measured at one location in Noda Village and nine locations in Miyako City. On the southern Sanriku coast in Miyagi, most of the 76 measurements range between 4 and 20 m. On the Ibaraki coast, 36 measurements range from 2.8 to 8.1 m, and the heights generally decease toward the south. On the Chiba coast, 43 measurements range from 0.7 to 7.9 m, with the maximum height near Iioka, Asahi City. |
| URI: | http://hdl.handle.net/2261/51526 |
| ISSN: | 00408972 |
| Appears in Collections: | 東京大学地震研究所彙報 東京大学地震研究所彙報
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