In this (time sensitive) image, one can see a large scale vort max embedded within the convection in E Central Arkansas, and associated trailing squall line extending SW to NE ... supercells are developing rapidly just out ahead of the main squall line, with embedded bow echos/segments, and LEWPS (line echo wave patterns) ...
tremendous divergence aloft continues to enhance the convergence at the SFC as depicted by anvil level winds ...
supercell composite yielding values as high as 8-10 in SW LA, and SE TX ... with significant tornado greater than 4 in a large area, with bullseye's exceeding 7 ...
Craven SigSvr Parameter (described by SPC in Norman, OK) ...
The simple product of 100mb MLCAPE and 0-6km magnitude of the vector difference (m/s; often referred to as "deep layer shear") accounts for the compensation between instability and shear magnitude.
Using a database of about 60,000 soundings, the majority of significant severe events (2+ inch hail, 65+ knot winds, F2+ tornadoes) occur when the product exceeds 20,000 m3/s3.
The index is formulated as follows:
C = (mlCAPE J/kg) * (SHR6 m/s)
For example, a 0-6-km shear of 40 knots and CAPE of 3000 J/kg results in a Craven SigSvr index of 60,000. Units are scaled to the nearest 1000 on the web plot.
And tonight we have a widespread area of >20 (or 20,000 m3/s3) ... and some bullseyes exceeding 60 ... (60,000 m3/s3.) ...
It will only continue to get uglier ... and if the nocturnal LLJ gets even more involved, potential F4's and a OUTSIDE POSSIBILITY of an F5 downstream towards E LA/C MS ...
SF