Dan Dawson
EF2
One thing that jumped out at me as I was looking at data tonight was the fact that the 0Z upstream soundings in the warm sector have a significantly deepr moist layer than what was advertised on the 12Z soundings. OUN AFD mentions this as well. Also, I really like the new 0Z Eta in that it holds the dryline a little further back from previous runs: still west of I-35 by 0Z. I really don't want to chase storms all the way into the woods of eastern OK again, so I like this development. Also, the directional shear, while not ideal, is still there, with about 30-60 degrees of turning from the surface to 500 mb most areas ahead of the dryline. Taking a closer look at the orientation of the dryline by 0Z, as the Eta advertises it, from central OK NW to the surface low in SW KS, the orientation is nearly SE to NW, unlike last Tuesday, where the dryline had a much more S to N orientation. Just eyeballing the sfc to 500 mb shear vector, this actually isn't a bad orientation, with the shear vector just ahead of the dryline being approximately S to N, or even a bit SSW to NNE. Thus, I'm a little more optimistic about longer-lasting discrete cells in central to northern OK, now that I've had a chance to examine the 0Z runs and data a bit more closely.