This is the mechanism how the wave is
formed. First, turbulent wind
flows form random pressure fluctuations at the sea surface. Small waves with a
few centimeters order of wavelengths is generated by the pressure fluctuations.
Second, the cross wind keep
acting on the initially fluctuated sea surface, then the wave become larger. As
the wave become larger, the pressure differences get larger along to the wave
growing, then the wave growth rate is getting faster. Then the shear
instability expedites the wave growing exponentially.
After that the interactions
between the waves on the surface generate longer waves
and the interaction will transfer wave energy from the
shorter waves to the waves have slightly lower frequencies than the frequency
at the peak wave magnitudes, then finally the waves will be faster than the
cross wind speed.
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