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Boreal Climate Change Profile

Overall 32

Winter Resilience Score

More climate-resilient than 17% of Western resorts · 32% of all North American resorts

#126 of 152 in the West · #149 of 220 overall

What goes into it, compared with Western resorts:

  • Season length at +2°C 20% better than 33%
  • Rain on the snowpack at +2°C 40% better than 12%
  • Snowmaking weather at +2°C 10% better than 19%
  • Terrain orientation 30% better than 36%

* 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.

Boreal Climate Change Takeaways

  • Rain potential: About 12% of winter precipitation falls as rain today, rising to about 37% with 2°C of warming. Ranks #129 of 152 Western resorts for rain resilience (#171 of 220 overall).
  • Season length: About 145 naturally skiable days a season today (Nov–Apr); about 112 with 2°C of warming (33 fewer).
  • Snow preservation: Terrain faces mostly northwest and gets about 9% less winter sun than neutral terrain. Its orientation holds snow better than 38% of Western resorts (35% of all North American resorts).
  • Base area viability: Moderate: the 7,200' base has about 141 naturally skiable days a season today, about 102 at +2°C.

Boreal Rain Resiliency Score

22

Less rain risk than 15% of Western resorts · 22% of all North American resorts

#129 of 152 in the West · #171 of 220 overall

About 12.5% of winter precipitation falls as rain today, about 37% at +2°C.

How well Boreal'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)
7,700' Peak 7.8% 8.8% 16.5% 29.4%
7,450' Mid 10.8% 12.1% 22.0% 36.1%
7,200' Base 14.8% 16.3% 27.9% 42.0%

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.

Boreal Season Length

145 days

More naturally skiable days than 36% of Western resorts · 55% of all North American resorts

#97 of 152 in the West · #99 of 220 overall

145 of 181 possible days today (Nov–Apr), about 112 at +2°C.

How many days a season Boreal 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)
7,700' Peak 150 141 125
7,450' Mid 147 134 116
7,200' Base 141 126 102
Skiable by Christmas 82% → 46% of winters with a skiable base on Dec 20, today → +2°C
Rain-on-snow days 5.3 → 11.1 per season with real rain (5+ mm) falling on the snowpack — slush, then ice
Snowmaking hours 660 → 420 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 Boreal's average snowfall. Melt follows the sun on Boreal'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.

Boreal Snow Preservation Score

−9% less sun

Terrain holds snow better than 38% of Western resorts · 35% of all North American resorts

#93 of 150 in the West · #140 of 216 overall

Boreal's runs get 9% less winter sun than the same slopes would facing every direction equally. Typical resort: 17% less.

How well Boreal'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 76 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.