It's a tug-of-war between low-level frictional convergence & strong horizonal shear near the FL panhandle plus the already somewhat prominent surface trough extending all the way into GA vs diabatically-forced surface pressure falls underneath the sheared convection out over the Gulf of Mexico. Both are competing for surface vorticity generation and upward motion and I'm not sure who will win although I'd lean ever so slightly to the Euro camp given its performance thus far (GFS didn't even have the low into the Gulf into a few days ago & kept taking the system out to the NE, the ECMWF in earlier suites was effectively showing what consensus is now). The GFS didn't have the convection that's now firing over the Gulf while the Euro was underselling the surface trough to the NE. Tough call really, I personally would like the northern solution to pan out to give more of the board some much needed rain and diminish the severity of direct impacts. Comes down to mesoscale processes that are exceptionally difficult to forecast and ones we have limited understanding of.