WARM   FRONTS
Dec 12 Dec 13
Dec 14 Dec 15
Surface Analysis
Dec 13 Dec 14
Jet Stream
Dec 13   0800 Dec 13   1200
Dec 13   2200 Dec 14   0800
Satalite - Radar Images
Barometer / Tempature
Wind Shift
Warm Front Passage

The passage of a warm front which consists of bubbles or pockets of warmer air in various sizes emanating from a low pressure system can bring a sudden rise in temperature at the surface over which it is passing.

With the advent of computerized weather stations these bubbles of warm air passing over such a station can be caught by the weather instruments and stored for later viewing.   Such an event accured at my station suddenly on December 13, 2001 at around 10 PM.   I was getting ready to quit for the night and was resetting my temperature gauges for the day when I notice that the temperature had risen substantially in the passed hour.   Upon checking the temperature plot from the computerized weather station I discovered that I had recorded a beautiful bubble of warm air passing over head in the past hour.

From the previous days downloads of weather images off the Internet I knew that there was a low pressure system passing to our northwest into Canada, and that there had been warm fronts developing around it.   The surface analysis and jet stream charts show this beautifully.   And as the graphs from my station shows, one of the pockets of warm air had passed directly over Chelsea, Vt and my instruments had recorded it’s passing.

The second graph also shows that there was a shift in the wind that directly coincided with the bubble of warmer air.   The blue lines indicate average wind speed and the purple ones give the direction of the wind.   At the same time the instruments showed that there was also a small bubble of high pressure which passed by during the next twenty four hours and brought a small amount of precipitation just before the entrance of a much colder air mass coming down from Canada the following day.

Without the capability of these new computerized weather stations to process and store the conditions taking place from minute to minute, many of these bubbles of warm air passing overhead would probably never be noticed, except that the high temperature for the day had taken place in the wee hours of the previous night.

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