Hi J.C.MacSwell
Thank you for the further elaboration.
My understanding of your explanation is that in the background, the boundary layer of air, which moves at 3 to 5 knots, is turbulent enough to break the surface tension on the water to a certain degree, such that it appears "lighter and smoother", while in the foreground, where the wind speed is 1 to 3 knots, the boundary layer of water is laminar as the water surface tension remains intact due to weaker wind energy. The difference in wind speeds between the two regions creates a wind shear where the air in the background rises up and over the air in the foreground. Additionally, similar effects can be noted in hurricane force conditions, where they can be read when a gust of upper airflow breaks the water surface tension and fans out pushing against the "relatively"(reason for quotation marks?) slower surface air that had established a more laminar boundary layer, even at those greater wind speeds and larger wave conditions.
Is my understanding right?
Also, does boundary layer refer to the surface of the water or basically the layer of air above the surface of the water? Or perhaps both, depending on specification?