Sunday, March 5, 2023

Blocked pattern to lead to chilly week with daily snow showers especially in northern areas and mountains; possible storm next weekend/early following week; more anomalous cold likely afterward

Plain-language summary:
 
A mostly quiet week is expected, with seasonably chilly not but particularly cold temperatures. However, it will be rather cloudy with snow showers from Tuesday to Thursday, especially northwest of the Appalachians. After a drier Friday and Saturday, a slowly-approaching storm from the west could transition to a Nor’easter for Sunday and the following Monday, but that is uncertain and it is too early for any details. It likely turns quite cold for March for the following week, with the potential for frequent snow showers and squalls, or even a true coastal Nor’easter.
 
Meteorological discussion: 

Behind the snowstorm yesterday, it is mostly quiet today, with a mix of sun and clouds for most except some mountain snow showers. It will be seasonably chilly today and tomorrow, but with no true arctic chill. A system heading into the northern Great Lakes will weaken and actually dive to our south Monday night, a symptom of the Greenland blocking pattern combined with a nearly stalled upper-level low over Atlantic Canada. The upper-level low will be too broad and far away to give us heavy precipitation, but Atlantic moisture wrapping around its northern and then western side, combined with a couple of shortwaves, will produce periods of light snow from Tuesday to Thursday, also a symptom of the Greenland blocking. The most snow will fall over the Laurentians, where the warm advection from the northeast is the strongest, and the northwestern slopes of the Appalachians, where there will be upslope enhancement. The flow will be somewhat blocked due to the warm advection above the cold low-level air, leading to the enhanced snow backing into the eastern Champlain and St. Lawrence valleys. The most widespread snow will occur Tuesday into Tuesday night. Areas near and just northwest of summits (especially the Green and White Mountains) could get 8-16” (20-40 cm) this week, with other areas receiving much less. 

Source: TropicalTidbits

As the upper-level low slowly moves to the east after Thursday, high pressure will settle to the northwest, leading to continued northerly flow and cold advection, though again there is no arctic chill to bring down. Daytime high temperatures will still be above freezing in most lower elevations if there is any sunshine, given the March sun angle. A storm will be slowly approaching from the west this weekend and could spawn secondary coastal cyclogenesis and turn into a Nor’easter by next Sunday or the following Monday. The slow movement is due to the blocking pattern. Such blocking patterns can be great for coastal snowstorms, but like has been the case for the entire winter, this does not appear conducive for a true big Nor’easter due to the ever present -PNA forcing the trough to dive into the western U.S. initially and then mature in the Plains and Midwest U.S. before shearing out over the persistent Gulf of Mexico ridge. Like almost every storm since late February, it would probably weaken as it heads southeastward before possibly re-strengthening along the East Coast. With the Greenland blocking, very strong western Atlantic trough, and not much of a northern disturbance to give it an additional boost, it could just slowly slide off to the southeast and slowly strengthen, preventing heavy precipitation across most of the northeast U.S. However, if the system is a little stronger with a weaker western Atlantic trough, heavy snow would encompass more of New England, and a lot can change in a week.

Source: TropicalTidbits
 

After that potential storm, more Bering Sea ridging and for once, a bit of a western U.S. ridge, will send more arctic air into the U.S. for the following week. While it will be modified by the March sun angle, and it will not be record cold, it could feel more like January or February, with any shortwaves producing short periods of light to moderate snow or even snow squalls. The upper-level pattern also might be more conducive for true coastal Nor’easter development and coastal snowstorms, but given how far out it is, ensembles only show a very vague signal for now, and it is getting more difficult, though certainly not impossible, to get snowstorms in southern and coastal areas.

Source: TropicalTidbits

Source: TropicalTidbits

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