Not bad from RAH:
Meanwhile, the surface low will move through the area tomorrow
evening and off the coast early Thursday morning,
deepening rapidly
as it does so. As would be expected, strong cold
advection will
commence tomorrow evening with a
rain to snow changeover looking all
but certain for areas along and north of US 64. Partial thicknesses
would indicate the best potential for a changeover would be in the
06Z - 12Z timeframe, but that could occur a few hours earlier if we
get any sort of
CSI banding or intense snowfall rates to develop.
While some accumulations appear
likely (an inch or less) north of US
64, little if any accumulation is expected to the south where cold
air will arrive too late and
moisture will have run out by the time
it gets there.
Today`s probabilistic guidance from the GEFS has increased storm
total snowfall accumulations quite a bit but EC ENS is a bit more
reserved and more realistic looking. There`s a handful of factors
that would lend themselves toward lower snow totals. The lack of a
strong surface
ridge over eastern Canada is concerning and while
there is cold air
upstream, we`
d be much more confident in
significant snow totals if the
ridge was parked over Ontario vs
Manitoba. Secondly, the surface wave rapidly moves out of the area
and offshore, really only giving us a good 6 hours of snow potential
vs a slower moving system. Surface soil temperatures aren`t overly
cold either (40s) but that could be overcome with intense snow
rates.
Overall given the variety of solutions out there, erring on
the lower end of the distribution seems to be prudent at this time.
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