Have you heard of the dry line before? If you live in the Texas Panhandle or Oklahoma, this is nothing new to you. Every spring, the dry line is talked about on severe weather days. So, what is it exactly and how does it relate to thunderstorm development?
The text book definition of the dry line is that it is a boundary separating dry and moist air masses. There is a very sharp definition between the air in this area. When looking at a weather map, you can find it around the 55°F dewpoint line. In the image below of dewpoint, you can see a thin yellow line separating the green moist air from the dry brown colored air in the Great Plains. This is the dry line!
Dry line magic occurs when storms form along this boundary. This doesn't happen without some assistance from an upper air system and forcing which leads to instability. Warm air ahead of the dry line rises and, if the conditions are just right, forms a rotating, severe thunderstorm. These storms form either on the dry line or right ahead of it. It is not unusual for these storms to be isolated and become supercells producing tornadoes.
It is common for the dry line to progress eastward during the afternoon hours and then retreat during the night. Therefore, storm development is not limited to daytime hours. In the following RadarScope loop, you can see the dry line retreating through Midland, Texas as the cold front advances. When these two boundaries meet, additional storms form quickly into a squall line.
#GOES16 captured this amazing infrared imagery of last night's powerful storms in the central US! See more loops @ https://t.co/z0YAKzuaYj pic.twitter.com/UIjdv2KxDr
— NOAA Satellites (@NOAASatellites) May 17, 2017
The dry line can often be found in the Great Plains in the spring. Just because it exists, it doesn't automatically mean severe storms will form. However, next time you see radar or satellite imagery showing a line of single storms with tornado warnings in Texas or Oklahoma, look for the dry line. You'll probably find it nearby!