weatherguy425 wrote:Guys, he's saying that most of the precip totals are coming from the rain along and ahead of the front, and a sooner front arrival would just mean an earlier onset to the squall line and would have little affect on frozen accum.
Right, but it DOES depend upon your location. For example, we have to consider the orientation of the cold front. What we expect to happen is for frontogenesis (a front to form) on an east-west orientation across southern Oklahoma early on Thursday. As the upper-level trof moves in later on Thursday, heavy precip breaks out in advance of it. A wave/low will form along the east-west oriented frontal boundary and the cold air will rush southward from the Texas Panhandle into west Texas. From the wave/low, the front will extend to the southwest. East of the low, the front will be oriented east-west.
So OKC-AMA will be in the cold air from the start, as frontogenesis will occur to the south of these two cities. The D-FW area would be south of the developing frontal boundary - in the warm air - when the heavier precip moves across. The only way there could be a significant winter event farther south is if the frontogenesis takes place farther south, because once that NE-SW oriented front trailing out the back side of the low/wave moves through D-FW, for example, that means the upper-level trof is moving through and there isn't much moisture to work with in the cold air.
What governs the location of the frontogenesis? It's the path of the upper-level vorticity center. So we're not watching for the front to move south faster than forecast, as it's not really there yeet. We're looking for a change in the path of the mid to upper-level energy that would shift the frontogenesis zone southward.