Affiliation:
1. Lomonosov Moscow State University
Abstract
An experimental study of the effect of wind blowing a wave induced by a wave generator in a direct channel
has been carried out. It is shown that at low wave steepness 𝑎𝑘 < 0.1 and wind speed 𝑊 < 2.3 m/s, a drift
current occurs on the water surface due to the influence of viscous forces. A formula for calculating its velocity
is proposed. It is found that the phase velocity of the wave increases with the appearance of a drift flow and
can be calculated using the formula obtained for linear waves on a flow with a constant velocity shift. With
an increase in the steepness of the wave 𝑎𝑘 > 0.19 and an increase in wind 𝑊 > 2.3 m/s, the formation of a
vortex deforming the water surface was detected in the air flow above the top of the wave crest. The vortex
destroys the viscous layer, reducing the drift velocity. At the same time, the phase velocity and wavelength
decrease. A mechanism explaining this process is proposed.
Subject
Space and Planetary Science,General Physics and Astronomy,Astronomy and Astrophysics