Tsunami run-up heights of the 2003 Tokachi-oki earthquake
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 Toka...
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| Veröffentlicht in: | Earth, planets, and space planets, and space, 2004-01, Vol.56 (3), p.359-365 |
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| creator | Tanioka, Yuichiro Nishimura, Yuichi Hirakawa, Kazuomi Imamura, Fumihiko Abe, Ikuo Abe, Yoshi Shindou, Kazuya Matsutomi, Hideo Takahashi, Tomoyuki Imai, Kentaro Harada, Kenji Namegawa, Yuichi Hasegawa, Yohei Hayashi, Yutaka Nanayama, Futoshi Kamataki, Takanobu Kawata, Yoshiaki Fukasawa, Yoshinobu Koshimura, Shunichi Hada, Yasunori Azumai, Yusuke Hirata, Kenji Kamikawa, Akiyasu Yoshikawa, Akifumi Shiga, Toru Kobayashi, Masaki Masaka, Seiichi |
| description | 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 Tokachi-oki 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. |
| doi_str_mv | 10.1186/BF03353065 |
| format | Article |
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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 Tokachi-oki 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.</description><identifier>ISSN: 1880-5981</identifier><identifier>ISSN: 1343-8832</identifier><identifier>EISSN: 1880-5981</identifier><identifier>DOI: 10.1186/BF03353065</identifier><language>eng</language><publisher>Heidelberg: Springer Nature B.V</publisher><subject>Capes (landforms) ; Earthquakes ; Edge waves ; Numerical simulations ; Seismic activity ; Tsunamis ; Wave propagation</subject><ispartof>Earth, planets, and space, 2004-01, Vol.56 (3), p.359-365</ispartof><rights>The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2004.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a616t-2a12b7ea8f02aed2423d757cf4d048ba161c91612b6a3332ee4bb5166cdb36613</citedby><cites>FETCH-LOGICAL-a616t-2a12b7ea8f02aed2423d757cf4d048ba161c91612b6a3332ee4bb5166cdb36613</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Tanioka, Yuichiro</creatorcontrib><creatorcontrib>Nishimura, Yuichi</creatorcontrib><creatorcontrib>Hirakawa, Kazuomi</creatorcontrib><creatorcontrib>Imamura, Fumihiko</creatorcontrib><creatorcontrib>Abe, Ikuo</creatorcontrib><creatorcontrib>Abe, Yoshi</creatorcontrib><creatorcontrib>Shindou, Kazuya</creatorcontrib><creatorcontrib>Matsutomi, Hideo</creatorcontrib><creatorcontrib>Takahashi, Tomoyuki</creatorcontrib><creatorcontrib>Imai, Kentaro</creatorcontrib><creatorcontrib>Harada, Kenji</creatorcontrib><creatorcontrib>Namegawa, Yuichi</creatorcontrib><creatorcontrib>Hasegawa, Yohei</creatorcontrib><creatorcontrib>Hayashi, Yutaka</creatorcontrib><creatorcontrib>Nanayama, Futoshi</creatorcontrib><creatorcontrib>Kamataki, Takanobu</creatorcontrib><creatorcontrib>Kawata, Yoshiaki</creatorcontrib><creatorcontrib>Fukasawa, Yoshinobu</creatorcontrib><creatorcontrib>Koshimura, Shunichi</creatorcontrib><creatorcontrib>Hada, Yasunori</creatorcontrib><creatorcontrib>Azumai, Yusuke</creatorcontrib><creatorcontrib>Hirata, Kenji</creatorcontrib><creatorcontrib>Kamikawa, Akiyasu</creatorcontrib><creatorcontrib>Yoshikawa, Akifumi</creatorcontrib><creatorcontrib>Shiga, Toru</creatorcontrib><creatorcontrib>Kobayashi, Masaki</creatorcontrib><creatorcontrib>Masaka, Seiichi</creatorcontrib><title>Tsunami run-up heights of the 2003 Tokachi-oki earthquake</title><title>Earth, planets, and space</title><description>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 Tokachi-oki 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. 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| subjects | Capes (landforms) Earthquakes Edge waves Numerical simulations Seismic activity Tsunamis Wave propagation |
| title | Tsunami run-up heights of the 2003 Tokachi-oki earthquake |
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