In several models for waves on water of finite depth, a great variety of su
rface-elevation profiles for steadily traveling waves can be generated by a
spatial evolution law in which the time-like variable is one of the horizo
ntal space variables. This is the case for both linear and weakly nonlinear
models, including the Kadomtsev-Petviashvili equation (KP-II); Al the line
ar level, these waves correspond to steady oblique interactions of one-dime
nsional wave trains. The shape of the waves is determined in a similar way
in all cases - by initial data that specifies the wave slope along a single
line oriented either parallel or perpendicular to the direction of propaga
tion. As one application we compute a steady two-dimensional wake due to a
pressure disturbance moving at near-critical speed in a weakly nonlinear re
gime. We find that the disturbance can generate solitary waves traveling ob
liquely in the wake, a phenomenon recently realized experimentally and foun
d to be relevant to the safe operation of high-speed ferries. (C) 2000 Else
vier Science B.V. All rights reserved.