Boy, what an intriguing set up. I always enjoyed attempting to forecast these "boom or bust" type events where the big question is whether or not anything will develop; however, if anything does develop it would go up in a big way.
Obviously there is going to be a whole lot of juice available tomorrow, especially across OK. The 18Z NAM portrays widespread 70-75F dewpoints across pretty much the entire state. The 18Z GFS even has a corridor of 75-80F dewpoints from SC into E OK. This could be a bit extreme, despite the rapid green-up we've had, and a lot of recent rainfall. I attempted to use the SREF Plumes from SPC in order to get an idea for a good, reasonable range of values to potentially expect tomorrow. At Norman, in the afternoon, the model mean is 72F with most ensemble members anywhere from 69F to 76F and all ensemble members between 64F and 80F.
It seems reasonable to expect lower 70s dewpoints. With high temperatures forecast to be in the upper 80s to near 90, there should be a pretty large amount of instability.
The biggest problem appears to be a lack of very strong forcing. There will be a pressure trough of some sort stretching from the SW corner of OK northeastward into E KS. It doesn't appear to be a cold front per se as temperatures are relatively uniform on both sides of the front. I guess you could call it a dryline, because there is an obvious moisture gradient, but it doesn't really seem like one. In any event, the density differences shouldn't be too terribly huge and convergence is expected to be weak.
Additionally, 500 mb flow is zonal and any disturbance (if it IS there on the model) is not really discernable. The GFS seems to want to indicate very broad, but very weak rising motion over the Southern Plains in vertical velocity fields.
I know the cap will remain an issue with 700mb temperatures approaching 12C in SW OK and 10C pretty much everywhere in OK. But, the good news is that there appears to be no cap in the forecast soundings. The 21Z OKC forecast sounding from the 18Z NAM run uses about an 86/71 surface condition. It has no cap, but notably there is very little positive buoyancy below 700mb. The CAPE above the 700mb layer is pretty substantial. In any event, this signals a couple of things to me. (1) The setup will get much more volatile (especially tornado-wise) if a few locations can get dewpoints up around 73-75F as opposed to the lower 70s. (2) The tornado threat is somewhat lessened by the limited instability (and thus vertical parcel acceleration) in the lowest few kilometers. However, with massive amounts of CAPE in the -10 to -30C layer, giant hail would be a big concern.
In any event, I suspect that a lack of any substantial cap and the abundant instability will allow for some storms to develop. The weak forcing should keep things more isolated. Only time will tell, but it should be a chaseable event. Unlike Tuesday, I think the cap will be weaker tomorrow. The only problem is the warmer temperatures in the 850-700mb layer may limit tornado potential for a time. As the daytime hours wane, I think the ascent may help cool that layer some (suggested by NAM forecast soundings). Low LCLs and the high dewpoints, along with increasingly curved hodographs after dark may increase tornado potential, but the lack of a strong focusing mechanism could cause everything to fall apart.
Boom or bust at it's best
AJL