A rather potent mid level shortwave and surface low will cross
the eastern Great Lakes Wednesday night, exiting into New
England on Thursday. This compact, fast moving system will usher
much colder air back into our region and mark the start of a
much colder and more wintry pattern after a long period of mild
weather.
DPVA ahead of the mid level trough and a wing of warm advection
ahead of the surface low will support a few showers spreading
quickly from west to east across the region Wednesday evening.
Temperatures will rise into the low or even mid 40s from western
Oswego County westward Wednesday evening, so most of this will
initially fall as rain. The one possible exception is east of Lake
Ontario, where colder temperatures surface and aloft may support
some wet snow right from the onset. Given the warm temperatures, any
snow accumulation will be minimal through most of Wednesday night.
The one exception will be the higher terrain of the Tug Hill and
western Adirondacks, where initial colder temperatures and upslope
flow may support a few inches of accumulation Wednesday night.
Strong cold advection will develop late Wednesday night following
the passage of the surface low center, which moves almost directly
overhead. A period of deep wrap around moisture, strong DPVA with
the mid level shortwave, and developing lake instability will
support snow showers becoming more widespread late Wednesday night
and Thursday morning as temperatures drop rapidly below freezing.
The higher QPF amounts during this period will be closely tied to
terrain, with developing WNW upslope flow combined with increasing
lake instability providing enhancement. This will target the Tug
Hill Plateau east of Lake Ontario, and the Chautauqua Ridge, Boston
Hills, and Wyoming County east of Lake Erie. Both areas should see a
period of accumulating snow very late Wednesday night through
Thursday.
Later Thursday afternoon and Thursday night the orographic
enhancement will give way to a more pure lake effect signal as a
cold pool aloft settles over the eastern Great Lakes. This will
support lake induced equilibrium levels of 8-10K feet Thursday,
slowly dropping to around 6K feet by late Thursday night as
inversion heights lower. A favorably deep mixed phase layer will
reside within the cloud bearing layer, supporting large, fluffy
dendrites. Boundary layer flow will become northwest, supporting
fairly widespread snow showers and narrow bands of snow southeast of
the lakes.