
Looking down onto
Willoughby Lake, Vermont, one can see an array of wind gusts. The
gusts darken the appearance of the water. The stronger wind
creates a rougher water surface which reflects the sky
differently. The wind out of the North is
blowing generally towards the observer in the photograph. One can
see about 4 separate wind gusts as "fronts" perpendicular to the wind
direction. The gusts are separated by about 300 - 500 meters.
at the earth's surface (or water surface)
the air "piles-up" in bunches. Periodically the increase in air
density of a "bunch" becomes unstable and the bunch spills out creating
a turbulent gust front. The gust fronts propagate in the same
direction of the wind flow as one can see from the animation at
right.
Similar effects can
be seen with water flow - especially if a film of water with the proper
thickness flows over a relatively smooth surface such as rain water on
a street. See the photo at left. 