Plain-language summary:
Our region has missed most of the warmth encompassing most of the U.S. over the past week, and that will continue for this upcoming week until arctic air becomes more widespread in eastern North America on Thursday. Light snow will fall from eastern Ontario to northern New Hampshire through tonight, heaviest over eastern Ontario and with rain mixing in Champlain Valley and St. Lawrence Valley in northwestern New York. It will then be chilly and dry Monday before turning milder with light intermittent rain Tuesday night into Wednesday night, but true warmth and precipitation will be limited, with only a short period of light rain expected for most, perhaps starting as wet snow in the Laurentians. It then turns cold and breezy with scattered snow showers across the region, especially in higher elevations along and northwest of the Appalachians, as well as heavier lake-effect snow bands in parts of the Adirondacks and eastern Ontario on Thursday and Friday. It will dry and clear out next weekend, with by far the coldest temperature of the season thus far, especially at night. Beyond next weekend, the weather pattern will become very volatile with big temperature swings, tight temperature gradients, and storms with all wintry precipitation types likely. There is the potential for one warmer system with wintry precipitation changing to rain early to middle of the following week and another one or possibly two colder systems a few days afterward, but this is highly uncertain, and the details of temperatures, precipitation amounts, and precipitation type will not be known until a couple of days before each system.
Meteorological discussion:
Our region missing out on warmth farther south, light snow today and tonight mostly New Hampshire on northwest
Despite most of the U.S. having unseasonable warmth over the past week after the previous week's arctic blast, a persistent northwesterly flow of chilly air has blocked any of the warmth from reaching our region. Over the past week, our region has some of the coldest temperature anomalies of all of eastern North America.
Today will continue that theme, with a weak Alberta clipper bringing light snow through tonight from eastern Ontario to northern New Hampshire, with rain mixing in for lower elevations of the Champlain Valley and St. Lawrence Valley in northwestern New York. The snow will be "heaviest" in eastern Ontario, where locally 5+ cm could fall, but amounts will taper off heading east as the system weakens.
Chilly and dry Monday, then turning milder through Wednesday night with period of light intermittent rain for most
A re-inforcing shot of cold and drier air will follow briefly for Monday, but that will not last long as a strengthening storm will push from the Rockies into the Great Lakes and into central Quebec Tuesday and Wednesday, bringing southwesterly flow into the region. While the initial cold air and lack of strong southerly transport of warm and moisture from the Gulf of Mexico will once again limit the intensity of the warmup (as well as precipitation intensity and duration) in our region, it will be warm enough for rain except in the Laurentians where light wet snow is still possible at the onset as the low-pressure system passes to our north on Wednesday. Precipitation will be relatively light and intermittent.
Cold with snow showers Thursday and Friday, heavier in lake-effect snow bands
An arctic air mass will blast into the central and eastern U.S. on Thursday and Friday, more powered by a -EPO and upper-level ridging in Alaska than ridging in western North America or high-latitude blocking, with the PNA, NAO, and AO all remaining near neutral. But with the low-pressure system over central Quebec, the cold air will first dive into the northern Plains and Upper Midwest U.S. first before heading eastward into our region, being modified over bare ground and the Great Lakes, so it won't be exceptionally cold when it reaches our region. Still, it will be colder than average for late November, and the wind will make it feel colder. There will also be lake-effect snow bands off the still warm Great Lakes, with the Lake Ontario band extending into the Adirondacks and possibly far southern Quebec, and the Lake Huron band extending into eastern Ontario. The general cyclonic circulation and lingering moisture will also lead to snow showers regardless of lake-effect snow, especially in higher elevations along and northwest of the Appalachians, though with much less accumulation than locations in lake-effect snow bands.
Very cold and dry next weekend, then likely milder middle of following week with any wintry precipitation potentially changing to rain, though still rather uncertain
By next weekend, an Arctic high-pressure system will be parked over our region, leading to any snow showers and clouds dissipating. Combined with lighter winds, low sun angle, and for some, still remaining snow cover, the coldest temperatures of the season so far by far will occur, especially at night. However, the PNA will then turn slightly negative, and most ensembles show a rather strong upper-level trough moving into the western U.S. With all the arctic air available, a lot of snow will fall in the Rockies and Plains, but if the system is too amplified, it will foster a strong downstream upper-level ridge in the southeast U.S. that would deflect the storm to our northwest, causing a quick warmup and precipitation type being rain except maybe starting as snow, ice pellets, and or freezing rain especially north of the U.S./Canada border, given how cold it will be ahead of the storm, especially in the low-levels. How all this plays out depends on the amplification of the weather pattern and if the system comes out in one strong piece or is split into weaker pieces, and we will not have much confidence on this until late next week.
Arctic air floods back in later in week, with potential for another storm, a potentially colder and snowier one but with very high uncertainty
Arctic air will flood back in as soon as the storm passes, though there could be another storm to slow the progression of cold air southward, especially if the southeast U.S. ridge is not beaten down much yet by that point. Temperatures and precipitation type will greatly depend on the exact timing and strength of these disturbances and connection to arctic air. At least one of the storms around that time (end of November into early December) will likely have access to both warm, moist Gulf of Mexico air from the south and arctic air to the north, straddling along the tight temperature and moisture gradient. This kind of setup is volatile and leads to very uncertain forecasts for any individual location, as a relatively small shift can make the difference between 50F (10C) with rain and 23F (-5C) with snow or the storm being suppressed too far south for any precipitation, leaving it just cold and dry. This kind of setup also leads to warm, moist air easily overrunning cold, arctic air, a setup ripe for a wintry mix of precipitation, with our region likely to experience all precipitation types (rain, freezing rain, ice pellets, and snow) at some point, perhaps even multiple times, with details not being known until a day or two in advance. Beyond that, ensembles show more upper-level troughing dominating in eastern North America with arctic air penetrating farther south, but that is uncertain given the PNA staying only near neutral. The most confident feature is the abundance of arctic air in mid-latitude North America given the continued upper-level ridging in Alaska, even without high-latitude blocking (which although usually promotes colder weather, can actually sometimes prevent the coldest air from being involved in the weather pattern).