The miller b looks to be sparked by a vignerons NS wave that’s fueled partially by the increasing thermal gradient as the true cold finally enters the N Amer playing field. But the wavelengths look wrong for us, it’s likely to amplify too far north. Forget the damn miller crap the issue is simple that wave won’t likely have the depth to get a storm under us. But as that wave amplified the cold will come behind. What happens after depends on a lot of factors. Currently the guidance favors the cold centering to our NW in a gradient pattern. That’s actually not a bad thing provided the blocking stays strong enough to keep the boundary to our south. We don’t want frigid into the Gulf of Mexico unless your goal is to walk across a frozen Potomac.