I know it's easy to get caught up in CWASP maps showing high values and models showing a good combo of respectable instability and favorable hodographs, but even if those things end up being present, there's still much much more to a significant severe weather event than that. You are very hard-pressed to get adequate moisture return when the western North Atlantic has the digging trough action just off the East Coast that it does. Sure, the GFS tempers this problem by being more progressive, but it is mostly out on a limb here in that regard. I had originally thought the Euro may be overdoing that troughing and how it lingers, but now that we are getting the NAM into the range of seeing how that troughing behaves out there Sunday night into Monday morning, it is closer to the Euro idea than the GFS idea.
But even if you hypothetically get a solution closer to the GFS where that troughing moves out and moisture returns adequately, there are other issues with the setup... such as a fairly significant plume of mid-level moisture overtop the warm sector, shortwave ridging overtop the low-level jet axis during the modeled "go time", and a meridional nature to the upper low with the main mid/upper jet core hanging back behind the surface front instead of crossing overtop the warm sector and intersecting the low-level jet axis. Things things all affect warm sector contamination, storm mode, and the ability to have enough large scale ascent in the open warm sector and low-level jet axis ahead of the front to develop sustained discrete storms.
Could Tuesday end up being a significant severe weather event? Yes, but the GFS is the most bullish solution, and even it has multiple problems on even the larger scale for a major tornado setup... much less trying to figure out smaller scale details that will ultimately make or break the event. Let's calm the hype a bit and step back to reality...