NWS-Philly office take on both the Monday system and the big storm for Weds/Thurs. For the big storm, they're highlighting the impressive model consensus/consistency so far and the steep snowfall gradient likely resulting from where the snow/rain line sets up - this could be one of those storms where ~50 miles from SE to NW is the difference between 1.5" of rain (with very little snow) and 12" of snow, with snowfall amounts increasing every mile to the N/W along that line (like from Belmar to Clinton for example) - we just don't know yet, where that transition will be.
Area Forecast Discussion
National Weather Service Mount Holly NJ
809 AM EST Sun Dec 13 2020
SHORT TERM /6 PM THIS EVENING THROUGH 6 PM MONDAY/...
Surface low pressure develops over the Gulf Coast this evening,
moves into the Southeast, and eventually towards the Mid-
Atlantic by daybreak Monday. The low will intensify as it moves
off the Mid- Atlantic coast on Monday as it moves out to sea and
towards the Gulf of Maine.
Most of the night will be dry. Precip will begin to nose its way
into Delmarva and far southwest portions of the Delaware Valley
prior to daybreak Monday. Temperatures will be below freezing across
the southern Poconos, far northwest New Jersey, and down into the
Lehigh Valley, and precip will be predominantly snow in these areas.
In general, 1-3 inches of snow will fall in these areas. A Winter
Weather Advisory may be needed for at least Carbon, Monroe, and
Sussex county, New Jersey if snow amounts end up a bit higher. Down
to the I-95 corridor, up to an inch of snow will fall in the morning.
The center of the low will pass south and east of Delmarva and
southern New Jersey. As a result, the rain/snow line will generally
be north and west of the I-95 corridor. So any snow over Delmarva
will change to rain through the morning, and precip will be rain
over much of central and southern New Jersey. Rain may even be
moderate to heavy at times.
Low pressure departs by Monday evening, and precip tapers off from
west to east.
Highs will generally be in the 30s and 40s.
LONG TERM /MONDAY NIGHT THROUGH SATURDAY/...
The main event of the extended begins to take shape Tuesday
night as a southern stream
trough centered over the southern US
progresses NEwrd, taking on an increasingly negative
tilt as it
does so. While the system`s initial surface low occludes and
lifts northward through the Ohio Valley, an initially weak wave
off the SE US coast, positioned along Monday`s stalled
boundary, will begin to intensify as the
shortwave & southern
stream
jet approach. This low will then lift NNEwrd through the
day on Wednesday, with the current consensus track taking it
very near the NJ/DE coast by Wed night/Thursday AM.
00Z Guidance retains rather impressive run-to-run consistency
with respect to timing, track, and associated
thermal profiles
with the low, and this is perhaps helped by the progressive
hemispheric pattern which tends to favor more predictability
than amplified blocking patterns. Consequently despite
considerable uncertainty regarding the details of this system
(more on that below) do have higher than average confidence that
at least portions of our area will see potentially significant
impacts from this system. The one thing to point out is that the
mid-
lvl wave associated with this system is still over the
Pacific which does favor at least some caution in becoming too
confident although modern Data Assimilation is fairly robust
even in regions of observational sparsity.
In terms of timing, did not make many changes from the previous
forecast, and see precipitation beginning to move into our area
Wednesday morning, with precipitation increasing in coverage
and intensity Wednesday afternoon into Wednesday night as both
the
sfc. low and UL
jet streak approach. In general the EC and
its
ensembles tend to depict the slowest progression, with
notable precip. continuing into the day on Thursday, while the
remainder of guidance has precip largely coming to an end
Wednesday night.
Unfortunately (or fortunately if you look at it from my
perspective) it is too early to get specific about ptypes and
snow amounts, as the low`s track near to the coast will almost
certainly result in some ptype transition zone. Furthermore this
transition zone will
likely ebb and
flow as
mesoscale lift
(e.g. FGEN) results in dynamical cooling. That being said the
antecedent airmass does look primed for wintry precipitation,
with pre-storm dewpoints
likely in the single digits or low-
teens which should support some fairly notable wet-bulbing with
the first batch of precip. The question then becomes can the
intensity of the precipitation and associated dynamical cooling
become enough to offset the increasing warm
advection associated
with the low? The next question is how robust will
precipitation be on the back side of the low Wednesday night as
it pulls away from the area, and cold
advection begins? We
should have more answers to these questions in the next couple
days we enter the
Mesoscale model window.
Finally it is also worth mentioning that the latest guidance
does depict a rather tight pressure
gradient between the
Canadian High and the intensifying low. This could certainly
result in gusty winds, and locations near the coast could
require wind headlines depending on the low`s track/intensity.