Tsunami run-up heights of the 2003 Tokachi-oki earthquake

被引:0
|
作者
Yuichiro Tanioka
Yuichi Nishimura
Kazuomi Hirakawa
Fumihiko Imamura
Ikuo Abe
Yoshi Abe
Kazuya Shindou
Hideo Matsutomi
Tomoyuki Takahashi
Kentaro Imai
Kenji Harada
Yuichi Namegawa
Yohei Hasegawa
Yutaka Hayashi
Futoshi Nanayama
Takanobu Kamataki
Yoshiaki Kawata
Yoshinobu Fukasawa
Shunichi Koshimura
Yasunori Hada
Yusuke Azumai
Kenji Hirata
Akiyasu Kamikawa
Akifumi Yoshikawa
Toru Shiga
Masaki Kobayashi
Seiichi Masaka
机构
[1] Hokkaido University,Institute of Seismology and Volcanology
[2] Hokkaido University,Graduate School of Environmental Earth Science
[3] Tohoku University,Disaster Control Research Center, Graduate School of Engineering
[4] Akita University,Department of Civil and Environmental Engineering, Faculty of Engineering and Resource Science
[5] Kyoto University,Disaster Prevention Research Institute
[6] University of Tokyo,Earthquake Research Institute
[7] Meteorological Research Institute,Seismology and Volcanology Research Department
[8] National Institute of Advanced Industrial Science and Technology,Deep Sea Research Department
[9] Disaster Reduction and Human Renovation Institution,undefined
[10] Japan Marine Science and Technology Center,undefined
[11] Sapporo District Meteorological Observatory,undefined
[12] Japan Meteorological Agency,undefined
来源
Earth, Planets and Space | 2004年 / 56卷
关键词
The 2003 Tokachi-oki earthquake; tsunami height survey; tsunami numerical simulation; edge wave;
D O I
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中图分类号
学科分类号
摘要
Tsunami height survey was conducted immediately after the 2003 Tokachi-oki earthquake. Results of the survey show that the largest tsunami height was 4 m to the east of Cape Erimo, around Bansei-onsen, and locally at Mabiro. The results also show that the tsunami height distribution of the 2003 Tokachi-oki earthquake is clearly different from that of the 1952 Tokachi-oki earthquake, suggesting the different source areas of the 1952 and 2003 Tokachioki earthquakes. Numerical simulation of tsunami is carried out using the slip distribution estimated by Yamanaka and Kikuchi (2003). The overall pattern of the observed tsunami height distribution along the coast is explained by the computed ones although the observed tsunami heights are slightly smaller. Large later phase observed at the tide gauge in Urakawa is the edge wave propagating from Cape Erimo along the west coast of the Hidaka area.
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页码:359 / 365
页数:6
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