I haven't paid much attention to the models given that, until the 0z runs come in tonight, we're still looking >72 hours out. When it comes to specifics such as whether the dewpoint at AMA and DDC will be 54F, 58F, or 62F, I think we all could agree that model forecasts at >72 hours out shouldn't be taken too strictly.
My biggest concern regarding a potential significant tornado event on Saturday is moisture quality and depth. As others have noted, at the elevation of the TX and OK panhandles and western Kansas and Nebraska, lower dewpoints are expected compared to areas farther east (the dewpoint of a surface parcel will decrease naturally as the elevation increases). However, there have also been other events that have looked similar but that have not produced significant severe weather. We can debate Tds to death, but the "Td required" or "Td sufficient" to produce a particular level of severe weather will always vary from situation to situation. The depth of the moisture is important, the degree of turbulent mixing in the boundary layer is important (both by mechanical mixing by strong shear and convective mixing caused by buoyancy as insolation occurs at the surface), and the vertical virtual potential temperature profile is important, amongst many others. I've never liked the use of "magic numbers", so I won't continue any further.
Let's remember that forecasts are the opinions of others. Nobody is a perfect forecaster, nor should anyone think they are a perfect forecaster. As such, let's try to be less critical of each other. Everyone has been burned before. In addition, everyone chases for different reasons -- some chase for the sole purpose of seeing a tornado, while others chase to see any strong convection. It's a personal decision, and I don't think any motive is any more "hardcore" or is any better than another. Let's not try to make ourselves feel more "hardcore" by putting down those who may only want to chase on "big days". Live and let live, as they say.
The strong negative-tilt nature of the trough, which appears to the first such trough of the spring, argues for a very strong ageostrophic response as strong pressure falls occur downstream of the trough and vorticity maximum. The surface reflection and response to the strong disturbance aloft will seen in the backed flow east of the dryline. Depending upon the depth of the southeasterly and south-southeasterly flow, we may be able to mitigate the amount of mixing that occurs in the boundary layer, which may help keep dewpoints from dropping too much through the day (or it may at least help off-set the positive affects from advection). In actuality, I'm increasingly becoming a fan of days with SOME cirrus in the warm sector, since ci may help prevent an "overmixing" of the BL (preventing the BL from becoming too deep, which tends to reduce low-level shear as winds in a well-mixed boundary layer tend to be relatively vertically homogeneous).
With deep-layer shear on the order of 50-60kts out of the west in the OK and TX panhandles, we should see a discrete convective mode preferred (deep-layer shear vector normal to the dryline), largely aided by mid-upper level flow out of the west at the base of the trough. Model performance in the past few days has been quite good, but let's remember that we are still 72 hours before the event. Despite how things look now, we should all know that they can change quickly and unpredictably.
So again, my primary area of interest is in the OK and TX panhandle region. I'm not confiden