Sunday, February 11, 2024

Turns much colder and more seasonable with major snowstorm to affect central/eastern New England Tuesday; clipper likely brings light snow Thursday into Friday, then even colder for next weekend; possibly stormier the following week

Plain-language summary:
 
The very dry and increasingly warm weather across the region will gradually turn colder starting today and continuing through Wednesday, though it will not be particularly cold for February. A snowstorm will affect the southern Adirondacks to southern Maine on Tuesday, with it being mostly dry to the northwest. A clipper will likely bring light snow to at least southwestern parts of the region late Thursday into early Friday before it turns even colder for next weekend. Storminess will likely return for the following week and possibly last for several weeks, with it being potentially the snowiest and most wintry part of the otherwise lackluster winter so far.
 
Meteorological discussion:
 
After an incredibly dry and increasingly warm stretch over the past week, colder air will gradually move in starting today and continuing through Wednesday. However, in the process, a storm currently in Texas will move east-northeastward and strengthen. Its northward movement will be limited by upper-level troughing and confluence to the north and northeast, and the lack of a strong northern trough just to the west to pick up and sling the storm northeastward. However, these storms laden with Gulf of Mexico and western Atlantic moisture produce a lot of latent heat from condensation and convection, which can be difficult for models to resolve, and they often move farther north than models show just a few days in advance. Indeed, models have trended northward for the past couple of days, though not by much, and this still limits the heavy snow to the southern Adirondacks to southern Maine on south, with light snow just to the north, and nothing from the Champlain Valley on northwest. Such intensifying storms produce a frontogenetic band of very heavy precipitation on the northwestern side, typically farther northwest than models show, and it will be cold enough for any precipitation to fall as snow. A narrow area of 10"+ (25 cm) is likely in this area, but the fast movement of the storm will prevent truly epic snowfall amounts despite isolated snowfall rates of 2-3"/hr (5-8 cm/hr).
 
Source: Myself
 
 
Source: TropicalTidbits
 
 
 
Source: TropicalTidbits

After the storm moves offshore Tuesday night, cold but not really arctic air moves in directly from the north-northwest without modification over the Great Lakes, with dry conditions dominating for Wednesday and early Thursday except perhaps some lake-effect snow showers downwind (south-southeast) of the unusually ice-free Lake Champlain. A clipper will dive southeastward from northern Ontario and will potentially be aided by some energy coming from the Midwest U.S. later Thursday into early Friday, which likely will bring light snow to areas from a line from western Quebec to southern Maine on southwestward. Accumulations will be limited by the moisture-starved nature of the clipper, as with any system coming from the northwest, though cold temperatures mean that any precipitation that does fall will be efficient in producing snow accumulation. There is some chance that the system strengthens enough due to the boost provided by the Midwest U.S. energy to provide enhanced snow, more than is typical of a clipper, perhaps up to 4-6" (10-15 cm) in some areas, especially in southern and eastern Ontario, where the clipper is likely to reach peak intensity before weakening as it moves southeastward into eastern New England and then offshore on Friday.
 
Source: TropicalTidbits
 
 
There might be another weak clipper next weekend that tracks a bit farther north, into southern Quebec bringing widespread snow showers, especially north of the U.S./Canada border, before true arctic air comes in. This is associated with a piece of the polar vortex descending into Quebec, aided by the development of Greenland or high-latitude blocking (-AO) and Alaskan ridging (+PNA). The strong and deep northerly flow will also be dry and suppress any storms well to the south. However, by early the following week, the polar vortex will retreat back into central Canada, while the Greenland or high-latitude blocking will continue to make cold air readily available in our region. This occurs while the pattern will become less suppressive, with the PNA turning to neutral or slightly negative allowing repeated storms moving into the U.S. West Coast due to the energized subtropical jet stream typical of a strong El Niño to then be more able to track across the U.S. and then up the U.S. East Coast, with some of the moisture-laden storms likely to affect our region. Long-range ensembles indicate that this could continue for several weeks, with an increased potential for Nor’easters and snowstorms, especially in interior areas. If things align correctly, this could be the snowiest and most wintry period of the otherwise lackluster winter thus far.
Source: TropicalTidbits
 
Source: Climate Prediction Center

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