NittanyLion, on Nov 6 2011, 11:00 AM, said:
Interesting event this morning if you're into radiational cooling. VERY shallow inversion layer observed this morning across the western half of Vermont. Coming into the office this morning, I left my apartment in the base of the Winooski Valley (~300 feet) with a temp of 23F. Drove westward up in elevation out of the Winooski Valley into Williston where the elevation is 500 feet, and the temp skyrocketed to 39F! Continued onward to where the office is in South Burlington (~350 feet), and the temp sunk back down to around 33F even though the Champlain Valley is much less prone to radiational cooling because of the lake and the terrain's various channelling influences increasing mixing.
Needless to say, when the sun came up, the inversion layer mixed out RAPIDLY due to its shallowness and at the office we were up to 45F by 9AM.
This map of our CWA shows it pretty well this morning:
You can clearly see the mountain valleys compared to the higher elevations. I put an oval around the Winooski Valley where the light blue colors (20's) are surrounded by the upper 30's in the higher elevations (21F vs. 37F). The warming provided by the lake is noticeable as well (39F).