Re. Baddour et Sw. Song, THE ROTATIONAL FLOW OF FINITE-AMPLITUDE PERIODIC WATER-WAVES ON SHEARCURRENTS, Applied ocean research, 20(3), 1998, pp. 163-171
Earlier analyses of waves on shear currents impose the stream profile
as a function of depth a priori. Nonlinear velocity distributions assu
med at the outset were considered by many authors. In the present work
we assume the existence of a stream function psi(x,y,t) unknown a pri
ori, for a stable, two-dimensional combined fluid how of a stream with
a free surface wave disturbance of finite wave length, periodic and o
f permanent type. The fundamental equations of motion and boundary con
ditions of the combined field are those appropriate to an inviscid, in
compressible fluid flow of finite depth with a free surface. The so-ca
lled current profile, i.e. y dependence, is unknown a priori, and not
imposed at the outset on the solution. We show that if the free surfac
e disturbance is assumed periodic and of unchanged form, then the reta
ined expression of the stream function is a quadratic in y, the vertic
al coordinate. First and second order wave undulations are developed f
or this case together with their corresponding dispersion relations an
d flow characteristics. (C) 1998 Elsevier Science Ltd. All rights rese
rved.