@article{oai:kansai-u.repo.nii.ac.jp:00010638,
 author = {Tanioka, Yuichiro and Nishimura, Yuichi and Hirakawa, Kazuomi and Imamura, Fumihiko and Abe, Ikuo and Abe, Yoshi and Shindou, Kazuya and Matsutomi, Hideo and Takahashi, Tomoyuki and Imai, Kentaro and Harada, Kenji and Namegawa, Yuichi and Hasegawa, Yohei and Hayashi, Yutaka and Nanayama, Futoshi and Kamataki, Takanobu and Fukasawa, Yoshinobu and Koshimura, Shunichi and Hada, Yasunori and Azumai, Yusuke and Hirata, Kenji and Kamikawa, Akiyasu and Yoshikawa, Akifumi and Shiga, Toru and Kobayashi, Masaki and Masaka, Seiichi and Kawata, Yoshiaki and 河田, 惠昭},
 issue = {3},
 journal = {Earth Planets Space},
 month = {},
 note = {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., The 2003 Tokachi-oki earthquake},
 pages = {359--365},
 title = {Tsunami run-up heights of the 2003 Tokachi-oki earthquake},
 volume = {56},
 year = {2004}
}