A 4-panel water vapor loop containing upper level (top left), mid level (top right), low level (bottom left) and the simple water vapor RGB (bottom right) depict a remnamt MCV from overnight convection making its way across the lower MO river valley, exiting the Omaha/Topeka CWAs. One interesting thing to note is the upper level anticyclonic rotation in the upper and mid level WV, while a cyclonic low level circulation is evident in low level WV imagery crossing northern MO. This gives a nice 3-dimentional picture of the MCF throughout the depth of the atmosphere.
Red-vis imagery shows a lingering boundary extending from central WI back through northern IA and into far northeast NE around 1930Z.
Comparing this with the day cloud phase RGB (above) shows only isolated cases of glaciation along this boundary across northern IA, and no glaciation noted across northeast NE. Will keep an eye on this product to see if an increase in glaciation can be noted across NE over the next couple of hours.
-64BoggsLite
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