Plain-language summary:
After an increasingly mild, dry, but
rather cloudy period today through Tuesday, a slow-moving storm will bring widespread
light to moderate rain across the region Wednesday with unseasonably mild
temperatures. Rainfall will be far less than last Monday’s storm. Precipitation
will lighten and likely change to intermittent snow by Friday before it dries
out by late in the weekend and early the following week. No major storms are expected
for a while afterward, but the colder air and northerly or northwesterly flow could
bring moisture-starved clippers that bring light snow, especially along and
west or northwest of the Appalachians. It is likely that eventually, the El Niño-enhanced
subtropical jet will bring storms with more moisture into our region.
Meteorological discussion:
With ridging dominating eastern North
America, it will be dry today through Tuesday and getting increasingly mild. As
is often the case at this time of year when it is mild with broad ridging,
there will be rather light winds with moisture trapped underneath an inversion,
leading to low clouds that don’t break up easily due to the very low sun angle.
During this time, a storm will slowly move east across the central U.S. and get
occluded and cut-off, with the slow movement being due to it being cut off from
the polar jet stream way to the north. The lack of the polar jet stream also
means that there will be no cold air ahead of the storm, and as the storm
arrives on Wednesday, it will be unseasonably mild in the whole lower
troposphere, and precipitation type will be rain, even in higher elevations, except
possibly from central Quebec to northern Maine. Since the storm will already
have occluded and is no longer strengthening, rainfall amounts will be no more
than moderate for most, unlike this past Monday’s storm.
| Source: TropicalTidbits |
However, this is a tricky setup, with
a broad cut-off low but multiple vorticity maxima rotating around and
interacting with each other. It is not clear how slowly the whole system will
move eastward. It could be already moving out by Friday if the polar jet stream
pushes into the storm by then, or if it remains removed from the storm, and the
storm strengthens a bit more and is more cut-off, it might not move out until
Sunday. It might also get buried to our south and leave us with dry high
pressure as early as Friday, as some recent model runs have hinted at. The GFS
model run yesterday morning (top) vs this morning (bottom) illustrates this
complexity and uncertainty. In either case, colder air will gradually move in from
the north and also will be manufactured in the upper-level low via ascent and
precipitation. The combination of these two should lead to most areas changing
over to snow by Friday, especially from the Appalachians on northwestward, as
it gradually gets colder, assuming that the upper-level low doesn’t get buried
too far south and dry it out completely. By the time the precipitation changes
over to snow, most of the moisture and strongest ascent will likely have passed
to the east, meaning that snow will be more intermittent and accumulations will
likely be light except in higher elevations. However, it is still possible that
one of the vorticity maxima spawns coastal low development that enhances
precipitation and snowfall in certain areas.