With surface heating underway (or soon underway) in southern Oklahoma, I think weak evapotranspiration and "dewpoint pooling" will be sufficient to raise surface dewpoints to the 58-60 range. Advection alone is certainly not going to do it with such weak wind fields! Those dewpoints will be quite shallow, as the regional soundings suggest 11 g/kg is the best we will be able to muster for the mixed layer.
So, given this idea, the fact I have the afternoon off and nothing better to do, I will probably wander on down to southern Oklahoma to play along the remnant boundary, perhaps where it intersects the weak/diffuse dryline. Deep shear is sufficient for supercell structure, but the high cloud base and poor low level shear suggests tornado potential would be limited to landspout-type vortices.
Target: Alma, Oklahoma (someone else already picked Velma!) 8)