Backdoor cold front season is here, what’s the deal?
Each spring we emerge from a long cold winter with aspirations of 70 degree temperatures, a cool breeze and plenty of sun. It rarely works out that way. Whether it be an upper level low, a stalled cold front, or a backdoor frontal boundary there are plenty of meteorological events that often are to blame for a colder and damp spring in this area. The fact of the matter is, our location during a transition season (fall, spring) is a difficult place to be. The changing and morphing wavelengths of the mid and upper level ridges and troughs mean the potential for cutoff lows, and the colder ocean waters this time of year especially will wreak havoc on any warmup.
This week, we will once again revisit the science behind a backdoor cold front. A significant low pressures system is forecast to develop through the Central United States during the middle part of this week, with the severe weather possible from the Plains into the Ohio Valley. Meteorology tells us that a warm front should be surging north from the Mid Atlantic states into New England as this low pressure moves towards the Great Lakes, with southerly winds ramping up warm air south of the front. But where is the warm front, and why hasn’t it made progress north? The answer lies in the setup both aloft and at the surface, and it leads to the development of a backdoor front which will push the warm air back to our south during the middle part of the week.