Originally posted by Damn Brit The fog has been pretty spectacular lately, or I just hadn't noticed it so much before.
On this evening last week, it looked just like an avalanche (or tidal wave) in slow motion.
I used slightly different processing according to what I thought looked best for each individual shot.
As usual, bigger versions in the gallery look better;
Gary, these are both beautifull and interresting.
There are lots of waves going on in the air. Usually you don't see them, but at the interface between cloud/fog and clear air you can see them.
A fog like this is usually trapped below an inversion, where the air is stable stratified. When something starts a vertical motion up or down, it is resisted by the stability and a buoyancy force counteract the motion, it goes the other direction, and meet an oposite buoyancy force and voila, you have a wave motion. Rising air find itself surounded by warmer air which force it to sink again and vice verse.
The cause of the initial motion can be mountains/hills/coastslines causing lee waves or mountain waves. There is alos something called gravity waves, which are a bit trickier to explain.
Was the wave building up in amplitude until it broke? In that case, what you most likely had in this picture, as far as I can judge from a still picture serie, is a Kelvin Helmholtz wave. Buoyance place a role here also, but it is the shear between a faster flowing air layer against a slower flowing air layer (remember that it is stratified in an inversion) that builds up until it gets strong enough to cause turbulence despite the stability which cause the wave to break. It is in principle what you have when the wind force ocean water to form a wave that breaks (also that is stratified "fluids", air and water). One can quite often see K-H waves build up at the top of fogs or clouds and break.
Sorry for the lecture. Could not resist.
Now imagine how nice it will be to have the K-7 next time you see this and to go over into video mode...