Tracking the "Super El Niño" and What It Could Mean for Next Ski Season

The Pacific is waking up.



The equatorial ocean is currently ENSO-neutral, but warm subsurface water has built for five straight months, and the atmosphere has started sending westerly wind anomalies across the western Pacific.



The current outlook gives El Niño a 61% chance of emerging from May through July and persisting through at least the end of the year, with winter outcomes ranging from neutral to very strong.



"Super El Niño" is the public label; the useful threshold is a Niño-3.4 anomaly of 2.0°C or higher, and that very strong outcome currently has roughly a 1-in-4 chance.



The whole setup still hinges on summer, when those westerly winds need to keep pushing warm water east across the tropical Pacific.



Keep reading for more on the impending "Super El Niño" and how it could affect the next ski season.

The Truth: Breaking Down a "Super" El Niño

For skiers, El Niño matters because it starts moving the storm track before the lifts spin.



During winter, El Niño pushes the Pacific jet stream south and farther east, loading more storm energy into the southern tier of the U.S. while the northern U.S. and Canada trend warmer and drier.



The classic North American map gives the Southwest, southern Rockies, Gulf Coast, and Southeast better odds for cooler, wetter weather, while the Pacific Northwest and parts of the northern tier carry a drier, warmer lean. Stronger ocean anomalies tend to give that pattern more weight, so a very strong event would make the seasonal map harder to ignore.



That does not turn winter into a vending machine. Mountains still make their own weather, and a single cold atmospheric river can bury a range that the seasonal outlook treated poorly.



The clean read is this: El Niño increases southern opportunity, raises snow-level anxiety in the maritime West, and weakens the usual La Niña comfort blanket for the Northwest and northern Rockies.



Skiers should treat the forecast as a directional edge, then let elevation, storm temperature, wind, and timing make the final call.

Where The Snow Wants To Go During El Niño

The upside sits south first.



High-elevation California, especially the central and southern Sierra, gets a better road into big storm totals when the subtropical jet lights up, though snow levels become the referee.



Mammoth, the San Gabriel and San Bernardino high country, Arizona Snowbowl, Taos, Wolf Creek, Silverton, Telluride, and the San Juans all deserve a closer look once the Pacific starts throwing pulses at the map. El Niño favors moisture before it favors blower powder, so the best skiing often comes on the colder back half of a storm, after the warm conveyor belt has soaked the lower mountain and stacked dense base up high.



Colorado gets split down the middle, as usual. The southern mountains can cash in when the jet tracks low, while the I-70 corridor sits in the messy middle, and the northern resorts lose some of the easy La Niña logic.



A Super El Niño year can make Wolf Creek look like a cheat code and still leave Steamboat waiting for the right northwest flow. That is the Colorado lesson every winter, sharpened by El Niño: follow the storm door, not the state line.



The Pacific Northwest carries the tougher setup. Idaho, Oregon, and Washington usually run warmer and drier during El Niño winters, with more precipitation falling as rain rather than snow. That is rough math for lower-elevation zones and coastal ranges, especially when freezing levels spike during warm storms.



Baker, Stevens, Hood, Bachelor, Schweitzer, and Sun Valley can still get hammered because the Cascades and northern Rockies terrain never needs much excuse to manufacture weather. The background signal simply asks more from each storm.

British Columbia and Alberta face a similar problem with a different accent. Whistler can still feast on Pacific moisture, but warm storms can drag the rain line into places skiers would rather keep frozen.



Interior B.C. and the Canadian Rockies need cold intrusions to turn a marginal pattern into a classic one. The colder the air mass, the less the El Niño label matters. The storm that arrives at 24°F writes a very different trip report than the storm that arrives at 35°F.



Back East, El Niño can feed an active southern jet and open the door for coastal storms when cold air is in place. The hard part is keeping that cold air in place long enough.



Interior New England, Québec, and the higher Appalachians should watch storm track and temperature profiles more than seasonal hype. A strong El Niño can deliver a memorable nor'easter cycle, a miserable rain line, or both in the same week.

How To Ski The "Super" El Niño

Build the winter around elevation and optionality.



A Super El Niño setup rewards skiers who can move late, chase cold windows, and read freezing levels as closely as snowfall totals. Big numbers in the forecast matter less when the first 5,000 vertical feet arrive as rain.



Dense snow up high can build an excellent base, but the powder window may sit above a nasty crust or behind a road closure.



The best bet is a flexible southern bias.



Keep the Southwest and southern Rockies high on the watchlist, keep California in play when storms run cold, and treat the Northwest with more caution than habit. Avoid locking every dream trip around a seasonal headline.



Watch the jet stream, snow levels, wind, and the cold side of each storm. That is where this winter's story will get written, one reset at a time.

Related: Alta Ski Area To End Season With Powder Day, 5-16 Inches Forecasted for Utah

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This story was originally published April 24, 2026 at 5:58 AM.