Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Satoshi Kusumoto"'
Publikováno v:
Progress in Earth and Planetary Science, Vol 10, Iss 1, Pp 1-9 (2023)
Abstract We examined whether it is possible to estimate the tsunami source model of the 2011 Tohoku-Oki earthquake from a comparison of numerical simulations of tsunami propagation and sediment transport, the measured trace heights, and the sediment
Externí odkaz:
https://doaj.org/article/34e275eb22e24f64a1e74197344523d8
Publikováno v:
Progress in Earth and Planetary Science, Vol 9, Iss 1, Pp 1-10 (2022)
Abstract We estimated the time difference between the 1854 CE Ansei–Tokai and Ansei–Nankai earthquakes from tidal records of two tide gauge stations (San Francisco and San Diego) on the west coast of North America. The first signals of the Ansei
Externí odkaz:
https://doaj.org/article/c84e8b4c18974641b554ffae3a625de5
Publikováno v:
Seismological Research Letters. 94:567-577
On 15 January 2022, an eruption of Hunga volcano generated an air-coupled tsunami that propagated across the Pacific Ocean. The tsunami reached Japan approximately 7 hr after the eruption and was recorded by coastal and offshore stations. We conducte
Autor:
Yuichiro Tanioka, Kentaro Imai, Karen Uno, Satoshi Kusumoto, Ryoko Obayashi, Narumi Takahashi, Takane Hori, Kenji Satake, Tung-Cheng Ho
Publikováno v:
Seismological Research Letters. 91:2624-2630
We estimated the origin time of the 1854 Ansei–Tokai tsunami from the tsunami waveforms recorded at three tide gauge stations (Astoria, San Francisco, and San Diego) on the west coast of North America. The tsunami signal is apparent in the San Fran
Publikováno v:
Progress in Earth and Planetary Science, Vol 9, Iss 1, Pp 1-10 (2022)
We estimated the time difference between the 1854 CE Ansei–Tokai and Ansei–Nankai earthquakes from tidal records of two tide gauge stations (San Francisco and San Diego) on the west coast of North America. The first signals of the Ansei–Tokai t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a16da00c807b3f31fef90a6a79b214b0
https://doi.org/10.21203/rs.3.rs-861187/v1
https://doi.org/10.21203/rs.3.rs-861187/v1
Publikováno v:
Marine Geology. 404:137-146
We found seven event deposits during the past 3800 years in a total of 16 geological core samples from a coastal lowland in Fukushima Prefecture, about 12 km north of the Fukushima Daiichi Nuclear Power Station. The event deposits consisted of well-s
Publikováno v:
Sedimentary Geology. 407:105740
We examined the effect of the coastal forest on tsunami sediment movement on the Sendai Plain, Japan, during the 2011 Tohoku tsunami using a numerical simulation of sediment transport. To account for the variable roughness coefficient in the coastal
Publikováno v:
Journal of Geophysical Research: Solid Earth. 119:4287-4310
Systematic tsunami traveltime delays of up to 15 min relative to the numerically simulated long waves from the 2010 Chilean and 2011 Tohoku-Oki earthquakes were widely observed at deep ocean tsunamimeters. Enigmatic small negative phases appearing be
Publikováno v:
TRANSACTIONS OF THE JAPAN SOCIETY OF MECHANICAL ENGINEERS Series B. 64:4193-4199
Autor:
Yoshimitsu Tajima, Satoshi Kusumoto, Ayumi Saruwatari, Tomohiro Takagawa, Yuki Sawai, Takahito Mikami, Nobuhito Mori, Shuji Seto, Kimitoshi HAYANO, Shunichi Koshimura, Tomoya Abe, Mohammad Heidarzadeh, Kazuhisa Goto, Shigehiro Fujino, Hitoshi Tanaka
Publikováno v:
Mori, N, Takahashi, T, 2011 tsunami survey team, T & Heidarzadeh, M 2012, ' NATIONWIDE POST EVENT SURVEY AND ANALYSIS OF THE 2011 TOHOKU EARTHQUAKE TSUNAMI ', Coastal Engineering Journal, vol. 54, no. 1, pp. 1-25 . https://doi.org/10.1142/S0578563412500015
At 14:46 local time on March 11, 2011, a magnitude 9.0 earthquake occurred off the coast of northeast Japan. This earthquake generated a tsunami that struck Japan as well as various locations around the Pacific Ocean. With the participation of about