Short answer- yes. Strength of HP does not mean it cannot get caught up in the flow and be transient. This is a huge common misconception that strong HP areas just can’t be moved, if there isn’t blocking, they will just keep on going. That being said, in this case we do have blocking. What we’ve seen shift is orientation. As the trough tends to dig further west, it is pulling our HP further north and opening up an escape path for our low to ride up the coast, in this case a miller B. Also while our HP is strong, the low has been trending stronger as well meaning it isn’t simply going to slide under the high. The high remains in an optimal spot for CAD areas so low level cold very likely will be there in the CAD favored regions throughout the storm but our storm system is likely still going to trend north as well as long as the trough keeps moving west. If I had to make a call now I’d say ATL has ice to rain, upstate has sleet to ice, SC midlands stay mostly ice, triad/foothills mostly sleet, triangle sleet to ice and coastal plain sleet to ice to rain. Snow will likely be limited to border counties and relatively brief. Think max snowfall might actually be in DC area up into Pennsylvania. Virginia likely gets thumped but I think with the coastal and miller b that warm nose changes the southern half over to sleet and eastern Virginia might actually be dancing with cold rain (Va beach, eastern shore).