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

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  • Tanioka Yuichiro
    Institute of Seismology and Volcanology, Hokkaido University
  • Nishimura Yuichi
    Institute of Seismology and Volcanology, Hokkaido University
  • Hirakawa Kazuomi
    Graduate School of Environmental Earth Science, Hokkaido University
  • Imamura Fumihiko
    Disaster Control Research Center, Graduate School of Engineering, Tohoku University
  • Abe Ikuo
    Disaster Control Research Center, Graduate School of Engineering, Tohoku University
  • Abe Yoshi
    Disaster Control Research Center, Graduate School of Engineering, Tohoku University
  • Shindou Kazuya
    Disaster Control Research Center, Graduate School of Engineering, Tohoku University
  • Matsutomi Hideo
    Department of Civil and Environmental Engineering, Faculty of Engineering and Resource Science, Akita University
  • Takahashi Tomoyuki
    Department of Civil and Environmental Engineering, Faculty of Engineering and Resource Science, Akita University
  • Imai Kentaro
    Department of Civil and Environmental Engineering, Faculty of Engineering and Resource Science, Akita University
  • Harada Kenji
    Disaster Prevention Research Institute, Kyoto University
  • Namegawa Yuichi
    Earthquake Research Institute, University of Tokyo
  • Hasegawa Yohei
    Seismology and Volcanology Research Department, Meteorological Research Institute
  • Hayashi Yutaka
    Seismology and Volcanology Research Department, Meteorological Research Institute
  • Nanayama Futoshi
    National Institute of Advanced Industrial Science and Technology
  • Kamataki Takanobu
    National Institute of Advanced Industrial Science and Technology
  • Kawata Yoshiaki
    Disaster Reduction and Human Renovation Institution
  • Fukasawa Yoshinobu
    Disaster Reduction and Human Renovation Institution
  • Koshimura Shunichi
    Disaster Reduction and Human Renovation Institution
  • Hada Yasunori
    Disaster Reduction and Human Renovation Institution
  • Azumai Yusuke
    Disaster Reduction and Human Renovation Institution
  • Hirata Kenji
    Deep Sea Research Department, Japan Marine Science and Technology Center
  • Kamikawa Akiyasu
    Sapporo District Meteorological Observatory
  • Yoshikawa Akifumi
    Sapporo District Meteorological Observatory
  • Shiga Toru
    Sapporo District Meteorological Observatory
  • Kobayashi Masaki
    Sapporo District Meteorological Observatory
  • Masaka Seiichi
    Japan Meteorological Agency

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抄録

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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