What a damn mess. ??
How can there be so many different solutions. I guess we need to hope the Euro comes in with the result it had earlier or it might be game over for a lot of us.
Closer to reality. I mentioned earlier this evening about how the warm nose can surge out of Statesville NC to Danville VA but struggle going west into Sparta/Wilkes counties. I think the snow maps were outrageously too high prior runs but now match what I said earlier exactly for the Charlotte metro region. Totals will pick up northern Mecklenburg back north west. Maybe 3-6” along i40 and 6-12” west of i77. Mixing could alter this by 2-4”.
How in the heck. It actually did better for North Alabama. There must be one skewed member in there.The snow mean on the GEFS definitely reflects a bit of a NW shiftView attachment 104209
There's support for a Miller B here but nothing asv extreme as the opView attachment 104210
View attachment 104211
Even if this takes a track up through TN, Alabama still does well especially if you have a ULL wraparound swinging south before shooting north. I think east of the apps would hurt if the gfs OP verified. That’s my 2 cents tho.How in the heck. It actually did better for North Alabama. There must be one skewed member in there.
Bingo. We have some Miller B members on the GEFS but they make it as far as central and northern Alabama before transferring to the coast. Which is actually a believable setup. The GFS OP just isn’t believable no matter how you slice it. The GEFS showed a clear picture of either a quick transfer without it pushing through the CAD or the southern members pivot around the CAD dome to the coast.The OP GFS doing GFS things again WRT to the first SFC low... some things never change with whatever version of it that's run.
Why in the hell does it take the first SFC low on a cyclonic trip directly to the mid/upper low and even ends up NW of its upper parent (*cough* BS *cough*) .. it shouldn't... but as GFS is as GFS does... already with that, it snowball effects and basically derails the rest of its prog...
cold air damming is extremely stubborn to scour, especially when it's reinforced with precip, latent heat aloft or not...
The parent high appears to be more or less in a really primed spot to stay entrenched for quite awhile ahead of the storm and the SFC low will still likely follow the wedge boundary... still be it, may Miller B but SFC lows don't bust through entrenched wedges quite so readily and the GFS is notorious for scouring wedges out too quickly..