What you’re seeing here are two different soundings.
The one on the right is the FV3, and the left side is the high resolution (3kmNAM).
The FV3 shows a nicely mixed PBL (likely means that radiative heating caused enough warm moist air to rise) which eroded the CAP and therefore intitiates convection, although the over mixing causes exaggerated updraft sizes which can balloon convective coverage.
Meanwhile the NAM has an over saturated PBL with no mixing to be seen, (which likely means there’s been little in the way of radiative heating/destabilization), and is CAPed all to hell. No convection can hope to trigger in that vertical profile.
When forecasting weather, its best to go with a mean. So I suspect there will be convective initiation, but coverage will be limited, but where ever supercells initiate, those will be capable of producing significant tornadoes.