Robert Dewey
EF5
I see where your coming from Rob. I don't get how the ETA can have a temp of 70F, dewpoint on lets say 56F, and cold air at 500mb, yet have such little CAPE?
Actually though, I have seen severe storms occur (mainly low topped, squall lines), with CAPES less than 500j/kg. An event such as this occured in December 6 of 1998 or 1999 right here in lower MI (your in Lansing, I think it may have developed just east of you). My location had a wind gust of 82MPH, and numerous trees were down over a widespread area. The temperature during that even was 45F, and obviously when temps are that low, dewpoints don't really matter. The squall line was mainly dynamically driven, which could be the case FRI for the Chicago area...
Robert
Actually though, I have seen severe storms occur (mainly low topped, squall lines), with CAPES less than 500j/kg. An event such as this occured in December 6 of 1998 or 1999 right here in lower MI (your in Lansing, I think it may have developed just east of you). My location had a wind gust of 82MPH, and numerous trees were down over a widespread area. The temperature during that even was 45F, and obviously when temps are that low, dewpoints don't really matter. The squall line was mainly dynamically driven, which could be the case FRI for the Chicago area...
Robert