@article{oai:kitami-it.repo.nii.ac.jp:00007767,
 author = {吉川, 泰弘 and 渡邊, 康玄 and 阿部, 孝章 and 大久保, 敦},
 journal = {河川技術論文集},
 month = {Jun},
 note = {This study aimed to clarify the pressure propagation velocity and pressure attenuation characteristic
of tsunami in ice-covered river. We carried out a hydraulics experiment for tsunami in ice-covered river.
This research clari ed the following things. The pressure propagation velocity of a  x-ice case is rapid
as compared with an open-water case and free-ice case. This velocity of free-ice case becomes later than
open-water case. In free-ice case, the pressure propagation velocity becomes late when ice-size becomes
smaller. The pressure attenuation of a  x-ice case is largest. If ice-size becomes small, pressure will not
attenuate. When ice-size is small, the dispersion wave train of the same phenomenon as open-water case
happens. On the other hand, When ice-size is big, It stops that dispersion wave train happens.},
 pages = {375--380},
 title = {河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性},
 volume = {19},
 year = {2013}
}