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Vail Climate Change Profile

Overall 84

Winter Resilience Score

More climate-resilient than 76% of Western resorts · 84% of all North American resorts

#35 of 152 in the West · #35 of 220 overall

What goes into it, compared with Western resorts:

  • Season length at +2°C 20% better than 91%
  • Rain on the snowpack at +2°C 40% better than 57%
  • Snowmaking weather at +2°C 10% better than 81%
  • Terrain orientation 30% better than 60%

* A ranking against the North American resorts we rate, not a grade out of 100: 100 = most resilient in the field, 50 = middle of the pack. Higher scores mean the resort's terrain and weather profile are more resilient in preserving winter conditions, both today and in a future of warmer temperatures.

Vail Climate Change Takeaways

  • Rain potential: About 2.8% of winter precipitation falls as rain today, rising to about 8.1% with 2°C of warming. Ranks #31 of 152 Western resorts for rain resilience (#31 of 220 overall).
  • Season length: About 165 naturally skiable days a season today (Nov–Apr); about 158 with 2°C of warming (7 fewer).
  • Snow preservation: Terrain faces mostly northwest and gets about 7% less winter sun than neutral terrain. Its orientation holds snow better than 28% of Western resorts (27% of all North American resorts).
  • Base area viability: Strong: the 8,120' base has about 158 naturally skiable days a season today, about 149 at +2°C.

Vail Rain Resiliency Score

86

Less rain risk than 79% of Western resorts · 86% of all North American resorts

#31 of 152 in the West · #31 of 220 overall

About 2.8% of winter precipitation falls as rain today, about 8% at +2°C.

How well Vail's winter precipitation holds up as snow rather than rain. We rebuilt 40 winters of hourly weather at the resort's base, mid-mountain and peak, then estimated whether each hour's precipitation fell as rain or snow from temperature and humidity. To see what warming would do, we re-ran the same winters 1°C and 2°C warmer. The score is a ranking, not a grade: 100 = least rain risk in the field, 50 = middle of the pack.

Rain % of winter precipitation, Dec 1 – Apr 15
i

1986–2006 2006–2026 +1°C rise*(mid 2030s) +2°C rise*(2050)
11,570' Peak 0.1% 0.1% 0.3% 0.7%
9,850' Mid 1.1% 0.9% 2.2% 4.6%
8,120' Base 6.0% 5.9% 10.0% 15.3%

The first two columns are the real observed weather record, split into two equal halves. * The +1°C and +2°C columns are stress tests: the full observed record replayed with that much warming added, so they show sensitivity to warming, not a forecast for a specific year. Elevations are rounded to the nearest 10 ft.

Vail Season Length

165 days

More naturally skiable days than 84% of Western resorts · 89% of all North American resorts

#25 of 152 in the West · #25 of 220 overall

165 of 181 possible days today (Nov–Apr), about 158 at +2°C.

How many days a season Vail has enough natural snow to ski, November through April. We simulated the snowpack day by day for 40 winters at the base, mid-mountain and peak — snow piling up, melting on warm days, and getting eaten away by rain — then ran the same winters 1°C and 2°C warmer.

Naturally skiable days, Nov 1 – Apr 30
i

Today +1°C rise*(mid 2030s) +2°C rise*(2050)
11,570' Peak 174 172 170
9,850' Mid 167 164 160
8,120' Base 158 155 149
Skiable by Christmas 99% → 96% of winters with a skiable base on Dec 20, today → +2°C
Rain-on-snow days 1.6 → 4.1 per season with real rain (5+ mm) falling on the snowpack — slush, then ice
Snowmaking hours 1,210 → 1,070 hours cold enough to make snow at the base, Nov–Dec
Why rain matters more than you'd think

Warmer winters don't just turn some snowfall into rain. Rain also eats away the snow that's already on the ground, in four ways:

  1. The rain itself is warm. This is the smallest effect — a soaking rain only melts a sliver of snow directly.
  2. Rainstorms bring warm, humid air. When moist air hits the snow, water condenses on the surface and releases heat. That's the main reason a single warm storm can wipe out a foot of base in a day.
  3. Rain primes the snowpack to melt. Cold snow soaks up rain and refreezes it, which warms the whole pack. Once it's soaked and at the melting point, every warm hour after that goes straight to melting.
  4. Rain wrecks the surface. Even when the base survives, rain leaves slush that freezes into ice. That's why we count rain-on-snow days separately — they hurt your ski day even when the snowpack doesn't disappear.

Our model simulates all four, using a simplified version of the snowmelt model the U.S. National Weather Service uses for river forecasting.

Natural snow only — no snowmaking or grooming, so resorts that make a lot of snow stay open longer than these numbers. “Skiable” means at least 3 inches of snow-water in the snowpack (roughly a 12–18 inch settled base). Snowfall is scaled to match Vail's average snowfall. Melt follows the sun on Vail's actual runs: shady, north-facing slopes hold snow longer than sunny ones. * Stress tests, not forecasts: the same winters replayed warmer. Checked against 40 years of real snowpack measurements at 105 SNOTEL stations across the West, where it's typically within about a week of the real season length.

Vail Snow Preservation Score

−7% less sun

Terrain holds snow better than 28% of Western resorts · 27% of all North American resorts

#108 of 150 in the West · #157 of 216 overall

Vail's runs get 7% less winter sun than the same slopes would facing every direction equally. Typical resort: 17% less.

How well Vail's runs are oriented to hold onto snow. North-facing slopes get less direct sun and keep snow longer; south-facing slopes lose it faster. We measured the direction and steepness of 241 mapped runs and compared the sunshine they receive with what the same slopes would get if they faced every direction equally, so this score reflects terrain orientation only, not latitude or elevation (those are covered by the rain score above).

Share of mapped terrain facing each direction. Trail data © OpenStreetMap contributors via OpenSkiMap.