"WeatherStowe, Vermont, stays in a light-to-moderate snow cycle through Thursday, goes quiet for a couple days, then turns milder with a more active and less certain mid-to-late week stretch. The best, driest refresh comes from today into tonight, followed by a small Friday night into Saturday system and a modest Monday night into Tuesday wave that brings slightly denser snow. The late-window storm potential increases from Wednesday into Friday, when snow levels rise and snow quality becomes more variable depending on timing and elevation."
"Wednesday-Thursday Snow Showers (02/11-02/12) bring the most reliable near-term refresh, focused on the upper mountain. Expect storm totals around 3″-4″ with snow levels near 0 feet, temperatures mainly in the low to mid teens °F, and SLRs generally 16-18:1, which supports fairly good, chalky powder. Winds run westerly to northwesterly 15-20 mph with gusts 35-40 mph, so exposed terrain near the summit can feel sharp while mid-mountain skiing stays more comfortable."
"Friday night into Saturday looks like a quick hit in the 1″ neighborhood, still cold enough for snow with SLRs near 16:1 and lighter winds around 10-15 mph with gusts into the 20s. Monday night into Tuesday brings another light 1″ with rising temperatures into the mid 20s °F, SLRs closer to 12-13:1, and snow levels around 200 feet, so snow quality trends denser."
Stowe will remain in a light-to-moderate snow cycle through Thursday with the most reliable refresh on the upper mountain. Expect about 3–4″ from Wednesday–Thursday with snow levels near zero, temperatures in the low-to-mid teens °F, and SLRs around 16–18:1 producing fairly chalky powder. Westerly to northwesterly winds 15–20 mph with gusts to 35–40 mph will make summit exposures feel sharp. A quick ~1″ arrives Friday night–Saturday with lighter winds, and another light ~1″ Monday night–Tuesday as temperatures rise and SLRs fall toward 12–13:1, yielding denser snow. Late-week storms (Wednesday–Friday) become milder and less certain, raising snow levels and making quality elevation-dependent.
Read at SnowBrains
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