Yes, the system strengthens rapidly because in an instant occlusion process at the large-scale a shortwave is rotating within the base of an upper level trough and the incipient disturbance catches up w/ a residual arctic frontal boundary and effectively strengthens the temperature (baroclinicity) and vorticity advection over it. Essentially what this looks like on satellite is you'll see (as we saw this morning) a baroclinic leaf cloud structure develop to the west of an elongated moderate-deep cloud mass and as time progresses, this will overrun this cloud mass associated with the arctic front and it'll eventually create a classic comma head structure to the storm that's often associated w/ stereotypical monster extratropical cyclones
Thank you. That makes sense. The new 12k NAM has a much, much more consolidated storm and is much closer to the coast than even the 18z HRRR, which is showing a decent precip shield inland. The 12k NAM has pretty much the same look as the 12z run. Still waiting on the 3k, but it looks like it's going to be as bad as the 12k.