SPC said 22000 thousand J/Kg CAPE.
Low-level lift and vorticity should be maximized near the boundary,
locally enlarging hodographs within an already favorable broader-
scale CAPE/shear regime for supercells. Diurnal heating along and
east of the boundary, rich low-level moisture (surface dew points
commonly upper 60s to low 70s F and 1.5- to 2-inch PW), and steep
midlevel lapse rates, will support MLCAPE from 1500-2500 J/kg over
north TX to 22000-3000 J/kg over the Hill Country and Rio Grande --
all amidst 50-60-kt effective-shear magnitudes. Though with weaker
moisture and deep shear, steep midlevel lapse rates and at least
marginal CAPE will support severe hail and perhaps gusts or a
tornado possible this afternoon and evening with convection
developing on either side of the cold front (west of the warm-sector
boundary activity) over OK and northwest TX.