MESONET TICKER ... MESONET TICKER ... MESONET TICKER ... MESONET TICKER ... January 16, 2001 January 16, 2001 January 16, 2001 January 16, 2001
The "Wet Bulb" Effect Shows up in Mesonet Meteograms
Several of today's Mesonet meteograms contain evidence of a significant "wet bulb effect", which can occur when precipitation falls into unsaturated air.
For example, today's Washington Mesonet meteogram
http://ticker.mesonet.org/archive/20010116/WASH.met.gif shows a 3-4 F decrease in temperature concurrent with a 6-7 F increase in dew point temperature at about 10:30 this morning. At the time, a very light winter mix was falling in central Oklahoma.
As the precipitation fell into the unsaturated air, it evaporated. This evaporation introduced water vapor molecules into the lowest layer of the atmosphere, which raised the dew point. Because evaporation is an endothermic process (it takes heat from the environment), it cooled the air.
On a shorter time scale, if you've ever felt a rapid but temporary temperature drop (say that three times!) during a snow flurry, chances are you experienced this effect, commonly referred to as the "wet bulb effect" or "wet bulb cooling".
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