Sea waves interacting with a surface current whose undisturbed velocit
y profile is linear form a physical system that is practically importa
nt and moreover easy to treat mathematically since the dispersion equa
tion becomes an algebraic equation The present paper emphasizes which
information about fundamental wave modes that can be obtained from gra
phical solutions of the dispersion equation. Use of Taylor's nondimens
ional variables Y = U/c and Z = hg/U-2 makes it possible to show in a
very clear way how the flow becomes unstable within a certain wave num
ber band. The instability is reminiscent of the Kelvin-Helmholtz insta
bility, but occurs even for a homogeneous fluid.