This looks like cap city to me from NE through OK, unless you're right on the dryline, at which point lapse rates are very good, but moisture depth is pitiful. It may be possible for a storm to form on the dryline and move out into the warm sector where CAPE and CIN are both greater. If the storm is well established with a very strong updraft, it may be able to survive the 50-100 J/kg of CIN that will be present and make for a nice looking supercell. I'd be surprised if there were more than one or two tornadoes out of this, although areas right along the boundary do show more than sufficient low-level shear for tornado production. However, these are still areas with either super steep lapse rates and no moisture or areas with a fairly strong cap.