B/H is different from mode of alternate bars (2)
Vorticity contours and the coherent structures above a deformed bed by NaysEddy.
Tsunami simulation of the Tohoku, Japan, 2011 by ELIMO
Solver: Nays2dFlood Simulated by Mr. Yoshiaki Ishida, Hokkaido University
Flood calculation on Asahi River, Japan by using SRM (Runoff calculation solver) and Nays2DFlood (2D flood cal
Solver: Nays2DH Simulated by: Dr. Tomoko Kyuka, Hokkaido University, Japan