Notice below the 500mb low (circle over the GOM, become an elongated trough reaching deep down into the GOm at 72 hours ... by this time, the MLC (yes, I will call it an MLC) will have already moved over land and with a very small to no opportunity to transition to "warm-core". However, I am NOT saying that a SFC low can't develop out of this, but it'll be due to baroclinic effects should this happen ...
The NOGAPS Ensembles show the same upper low elongate and merge with another trough coming from the west, and covers the Western 1/3 of the GOM ...
https://www.fnmoc.navy.mil/PUBLIC/EFS/j ... 00_sd.html
And only ONE or TWO of the CMC ensembles show ANYTHING resembling a potential tropical cyclone out of 16 members ... and the CMC2 is ALMOST ALWAYS overeager (like the GFS with convective feedback issues) to close off ... to take the cake, CMC2 and then merge with the oncoming trough and develop quite the extratropical storm system that would typically be seen in March or April ... discounted solution...





