Overrunning: How the 'cool clouds' formed
My inbox was flooded with photos Sunday evening, even more were shared on social media. Many posts were in awe and wonder of what were these clouds? I knew after seeing the first photo what was going on, as there was a front nearby, overrunning.
Ripples in the clouds along the stalled warm front.
— Tom Coomes (@TomCoomes) May 8, 2023
The warm air is trying to rise over the cooler air south to north. Each ripples is the next “ step” up the incline.
? Christa Risher #inwxpic.twitter.com/w28UAXvY3t
Sunday was a warm day but by the evening the cool air had started pushing southward, displacing the warm air. Cold air is heavier than warm air, so it wedges along the surface. The warm air is lighter and rides over colder surface air.
The surface boundary between warm and cold air, is lift mechanism for the atmosphere, and storms started forming along it. In fact, with the convergence of north / south wind along this stalled boundary, a stagnant line of flooding thunderstorms formed.
The clouds however kept rolling up over the wedge of colder air northward across Michiana.
The roll-up is not a smooth process, especially with storms, the wedge isn't exactly a knifes edge. The waves in the clouds were the evidence of folding of the atmosphere as it was forced to a higher altitude.
While pulling into my driveway, a better example hit me as I pressed the remote to open the garage door. As each panel rises is eventually bends at the hinge before turning horizontal. That's essentially what the atmosphere did, those ripples and crinkles were the atmosphere hinged higher.
Remember those cool clouds yesterday ? ☁️☁️☁️ I’ll tell you why they made me think of my garage door on Night Team #inwx #miwx pic.twitter.com/HRAylYAoDE
— Tom Coomes (@TomCoomes) May 9, 2023