Abstract
This paper provides a theoretical description of the 3-dimensional flow produced by a surface pressure distribution moving in a channel at speeds such that the Froude number based on depth is near 1. The transient flow begins in a fully 3-dimensional manner, then focuses away from the distribution, due to the side walls, into predominantly 2-dimensional “solitary” or “cnoidal” waves. Two sets of these waves are generated continuously by the distribution; one set runs upstream while the other extends downstream.

This publication has 3 references indexed in Scilit: