I think the less of a coastal impact there is the more that convective line moves east .. at least that tends to look like what the models portray
We are all going to be fighting over the 850/700mb convergence axis tomorrow to see who gets a dusting and who gets 1-3
They're used too big storms.40" for Boston on the NAM. This sounds like a good idea but after about 24 hours it's going to feel suffocating not being to go anywhere.
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I would appreciate it if you could explain what im watching. I assume those circles mean areas of alot of snow but not sure.If you are trying to throw a hail Mary for tomorrow evening with the coastal watch thisView attachment 111050
Watch or look at? Is it a video?I would appreciate it if you could explain what im watching. I assume those circles mean areas of alot of snow but not sure.
I would appreciate it if you could explain what im watching. I assume those circles mean areas of alot of snow but not sure.
Thanks. It looks like coastal areas and west NC could do quite well.In this case you might eek out a stripe of heavier precipitation that might be enough to change rain to snow where the 700mb warm front is starting to shapen up and close into the eventual 700mb low. You get a little warm adnvection in orange on the right and little cold advection on the left you start to have convergence and lift.
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You know the rule about snow maps. We hardly ever trend up into the storm. We hang on to the couple inch maps and end up verifying low. These kinds of bands die off as they move east, in most cases...not every case. If we see more than a dusting to .5", I'll be very shocked. We needed the coastal to work out. Folks west and southwest of the Triangle will probably pick up 1-3".
Maybe in the east the nam is excited about NE NC. We all have some dry air issues below 700mb and boundary layer temperature issues so even if we have an overperfoming band here some is going to go into moistenening the column and some of going to go into cooling the boundary layer as rainThanks. It looks like coastal areas and west NC could do quite well.
I think a wait and see attitude from RAH is a prudent call as of now. If the band dumping 2" to 3" over the western piedmont should continue moving east or the potential for wrap around snow from the coastal storm increases then advisories or watches and warnings may be needed. Until then, don't get the public flying to the stores to buy milk and bread before anything looks like a possibility.RAH just updated AFD. The question of WWAs will be the evening shift's problem:
With that said, the latest forecast now shifts the highest snowfall
totals across the western Piedmont, where the highest water-
equivalent is forecast and where the best potential for banding
exists. Expect most areas along and west of US 1 to see light snow
of 1 to 2 inches, with the potential for some very localized/focused
higher amounts over the western/NW Piedmont. Conversely, given the
trend of lower liquid amounts across the coastal plain with the dry
slot, snowfall totals are generally less 1 inch with the potential
for some locations to see as little as a dusting.
Given there is still quite a bit of model spread and forecast
uncertainty, will hold off on issuing any headlines with the
afternoon package, deferring in hopes that forecast confidence will
continue to increase upon review of the full suite of 00z/28 model
guidance.
Newfound gap special
If it shows snow, we like. However, have we ever seen the WRF end up correct?
And Virginia lolBand continues to get closer to wake county .. hmm ?
IMO globals just can’t be trusted at this rangeThe lee side low showing up on the 18Z GFS:
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Isn’t that the eventual replacement for the NAM? I don’t know if it’s good, but it does show snow for us, so we like it.
That is true. While global aren’t very reliable at this range they have been way more consistent than the NAMGFS/Euro have been locked in on CLT View attachment 111078
Rain for Belmont and Gastonia! Oof ?The lee side low showing up on the 18Z GFS:
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No that will not be rainRain for Belmont and Gastonia! Oof ?