Good
radiational cooling led to a low of 23F last night. It has clouded up,
but not as much as expected, with enough sun to mix out the very shallow
but sharp inversion somewhat, leading to a high of 46F, higher than
almost all models. The winds have been very weak too, with a maximum of
7-8 kt so far with a Chesapeake Bay breeze occurring now. The snow cover
is pretty much gone now. After an initial cooldown with decent
radiational cooling this evening with a bit of clearing and no wind,
thickening low-level clouds will stop the cooldown after 06z or so
tonight, leading to an early low. Tomorrow, a slow warmup will ensue,
greatly mitigated by thick low cloud cover and some cold air damming
east of the Appalachians. The high is expected to occur at the end
(Thursday 06z) with weak warm advection and clouds continuing. Some
models are suggesting that the southerly winds will get going at around
the end, which would lead to a sharp warmup around then, but I would bet
against that and lean cold given the tendency of shallow low-level cold
air like this to persist longer than model guidance, especially when
forcing to scour it out is weak like in this case (no strong low
pressure system or strong low-level jet). The GFS does appear a bit too
cold however. The cold, stable low-level air will also prevent the
southwesterly winds aloft from mixing to the surface, and winds will be
rather weak again. A few showers are likely in the afternoon or evening,
though it is expected to be intermittent and not much, with most of the
dynamic forcing staying to the north.
| Source: PivotalWeather |
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