I say the following while acknowledging that the ingredients are still there for a significant event. The 00z HRRR really goes bonkers with what looks like quite a bit of mature convection over the warm sector starting in the early afternoon, even if it's a little messy. However, 0-1 km SRH is under 200 m2/s2 for a lot of the area until the end of the run. I'm not saying this to downplay the threat, but I'm wondering if that could limit the higher-end ceiling of this event *until at least the evening/overnight round*, or if the higher-end thermodynamics and instability for the area could compensate. Or conversely, does anyone think that the wind fields and shear will just straight up be stronger than shown by the HRRR? I'm more used to Plains events having the instability and lacking huge shear, not really familiar with Dixie Alley climo in these circumstances, and I'm not an expert by any means.
Again, I stress that I'm not trying to make anyone put their guard down, because that run is still awfully worrisome. Just asking, because obviously a lot of the pretty high-end events (no, I'm not only referring to 4/27/11, of course) in the area that come to mind had notably more shear/SRH than this *one* run shows. I also insist that the end of the run brings more favorable shear across the threat area anyways, so even if storms in the afternoon don't materialize into widespread long-track sigtor producers, the later round still very well could have some, as this will likely be an event with several rounds, as has been widely discussed here already. Regardless, it would be best if the event weren't to verify to that extent.
EDIT: Oh well, another note, I should have thought this through more, but the afternoon part of the event is where boundaries left by earlier storms have a role, I would imagine. We could still have afternoon storms interact with boundaries that locally enhance the shear, even if widespread high helicity values aren't present.