Well, the NWS Raleigh discussion is discouraging to say the least. I will post the full discussion here because of the important information and things to take into considuration.
4:10am
What has changed: Reduced snowfall amounts a bit across the
southeastern zones and focused the peak accumulation amounts (1-2")
a bit further north and west to better coincide with latest model
trends. Our forecast remains much lower than most raw forecast
guidance due to
numerous limiting factors, including; (1) Warm
surface temperatures, (2) Self-limiting
CAA processes, and (3) Low
rain to snow liquid ratios. Impacts should remain rather minimal,
however, a few slick spots may form on area roadways during the
overnight hours Thursday into early Friday morning, primarily along
and east of US-1. If the forecast holds true, a Winter Storm
Advisory issuance may be needed in future forecast packages (Our
criteria is areas that are expecting to see 1" of snow or greater in
a 12 hour period).
Full Discussion: The surface
front will settle in a nearly west to
east orientation in vicinity of the SC/GA border, with ongoing
surface
CAA processes occurring north of the boundary. The
front is
progged to buckle back north as a series of weak disturbances begin
to develop during the day Thursday, with strong coastal
cyclogenesis
beginning to initialize off the SC coast as early as Thursday
evening. Around the same time, strong Canadian surface high pressure
will continue to settle southeast through the central Corn Belt
states, extending east through the Great Lakes and northeastern US
states before beginning to south along the
lee side of the
Appalachians.
Location and strength of the developing coastal low/
trough will be
key to the forecast going forward, as a stronger and closer to shore
area of low pressure (
NAM) will help to promote more rapid cold air
entrainment from the north. Forecast models continue to trend
increasingly more wet during the daytime hours Thursday, especially
from the US-64 corridor south during the afternoon and late evening
hours. Around this time, a 925mb cold
front (marking the leading
edge of the cold nose) will extend south into the area. This will
aid, at least initially, in the ability for wet bulb/evaporative
cooling processes to promote a light rain to snow changeover to
occur in vicinity of the VA/
NC border mid to late afternoon. From
there, a gradual changeover to a rain/snow mix to eventually all
snow will occur. At first, accumulations will remain little to none
with more of a "white rain" type scenario unfolding. Eventually,
especially areas east of US-1 where rain rates will remain higher
for longer, the wet-bulb effect will help to cool surface
temperatures below freezing, helping to promote accumulations
primarily on grassy and elevated surfaces. Best timing for this will
be between 02z/9pm Thursday through 10z/5am Friday morning.
Snow amounts continue to remain highly uncertain in this event,
however, thinking that raw model output remains way too high in this
scenario. Several limiting factors remain at work, including: (1.)
Persistent above freezing surface temperatures that will help
temper/melt the majority of the snowfall. The exception to the rule
may be areas closer to the VA/
NC border, however, these are the
areas that will
likely see far less
QPF throughout the event (2.)
10:1 snow to liquid ratios are not
likely in an event like this,
expect closer to 3:1 at precipitation changeover onset, 5:1 toward
the middle of the event, and perhaps ending in vicinity of 10:1 if
we are lucky. (3.) While the
CAA process will be key in the original
changeover, it will also become the ultimate limiting factor through
the frozen ptype portion of the event. Gradual drying is expected to
persistently take place in the lower-third of the
boundary layer as
the cold air slides south into the region. This will work to greatly
reduce
QPF from northwest to southeast in general. Higher amounts of
QPF in the southeast will remain, however, dewpoints in the middle
30s will keep widespread snowfall accumulations from occurring.
With these limiting factor in mind, have shifted the geographic
location of accumulations a bit further north and west. Amounts are
down a bit also with this run, topping out in the 1 - 2" range in
northeastern Coastal Plain. From there, if you follow the US-64
further west, expect accumulations in vicinity of an inch with
lesser amounts as you progress west of US-1 and south of US-64.
Alterations and fine tuning to the accumulation forecast is highly
likely to continue with sequential model runs and forecast packages,
but still finding it highly doubtful that significant snowfall
amounts will occur across central
NC. For the snow lovers out there,
the canary in the mine that could indicate the potential for higher
amounts lies in surface dewpoints Thursday afternoon. If dewpoints
become significantly cooler, a possibility advertised by the
recently cold-initialized
NAM, wet-bulb cooling processes may
promote an earlier changeover and perhaps higher amounts somewhere
across central
NC assuming the
moisture is available.