In this paper we report the results of the first laboratory study on t
he relationship between the initial growth of the shea wind waves and
the simultaneous development of the wind-induced drift current. The ph
enomenon of the first visible ripples appearing ''suddenly'' on the wa
ter surface and forming V-shaped streaks aligned with the wind is expl
ained. We show that the laminar-turbulent transition of the near surfa
ce water flow causes an explosive growth of the initial wind-generated
ripples. The grown ripples become visible and thus mark the surface o
f the well-localized V-shaped turbulent zones forming the streaks. (C)
1998 American Institute of Physics.