Sunday, any lingering synoptic precipitation will end early as mid
level moisture carries towards eastern New York and New England.
There will likely be a limited lake response south of Lake Ontario
Sunday morning as a weak surface trough drops southward, with
shallow cold air advection behind it. Light snow, mainly north of
the NYS Thruway could accumulate a fluffy half inch or so through
the morning hours before increased wind shear ends the lake bands
through the afternoon hours. This shallow cold air advection will
also lower the snow dendritic growth zone, such that any patchy
freezing drizzle late Saturday night may return back to just plain
snow, with added lake moisture.
There may be a few breaks in the clouds Sunday afternoon for some
sunshine, especially east of Lake Ontario. Any clearing will be
temporary as another system brings an increase in clouds through the
evening hours of Sunday.
Sunday night a deep long wave trough will dive well down into the
Southern Plains, with surface high pressure over the Western Great
Lakes. Meanwhile a surface low will advance northward along the east
coast...though remaining well offshore. This synoptic setup will
produce a baroclinic boundary that stretches from near Texas
northeastward towards New England.
A favorable jet streak over southern Ontario Canada will place the
right entrance region over our area, with a widespread but light
snowfall event unfolding late Sunday night and through the day
Monday. Greatest snowfall accumulations may lie near the Southern
Tier and Finger Lakes region where 850 hPa frontogenesis will be
strengthening. Several inches of snow will fall within this event,
with snow tapering off Monday afternoon and evening as the upper
level jet streak and mid level moisture pushes northeastward.
However, a second and much stronger jet will emerge from the Ohio
Valley Monday night, with the right entrance region of a 180 knot
250 hPa jet streak passing over our region. Additionally a shortwave
trough will pass across our region Monday night and into Tuesday.
Lower in the atmosphere a 60 knot LLJ will advance northward along
the east coast, with the left exit region nearing our region. This
LLJ will also aid in deeper Gulf of Mexico moisture transport from
the south...which combined with the increased lift from the
shortwave and jet could bring a heavier snowfall event Monday night
and through the day Tuesday.
There is still model uncertainty with the evolution of this event,
in particular the placement of strong low level moisture advection
and core of the LLJ. The 00Z ECMWF is a bit slower and westward with
the axis of low level winds...which would aid in accent and overall
snowfall accumulations, while the 00Z GFS is a bit faster with the
LLJ and eastward, which would lower the impacts from the jet
streaks for our region.
For now we will highlight the snow potential of at least a few
inches, possibly more (00Z ECMWF/some members of the 00Z GEFS
solutions) in the HWO product.