❄️ Satellite Ojisan — Resort Comparison

Resort Snow Comparison

How does La Niña / El Niño affect each resort differently? ONI-based seasonal snowfall predictions for Japan's top ski destinations.

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Current ONI index: Weak La Niña

La Niña strengthens the Siberian High, pushing cold air masses over the Sea of Japan → more moisture pickup → heavier snowfall on the Japan Sea side (Myoko, Nozawa, Madarao). Pacific side resorts (Hakuba Valley, Shiga Kogen) see moderate increases. Hokkaido benefits but less dramatically.

2026-27 Season outlook
Resort-by-resort comparison

ONI vs seasonal snowfall (30 seasons)

Negative ONI (La Niña) = more snow. The correlation is strongest for Sea of Japan side resorts (r = -0.73).

Why JAPOW is different: the science

The Siberian Express: Cold, dry air from Siberia crosses the Sea of Japan — one of the warmest seas at that latitude. In just 500-800km, the air mass absorbs enormous amounts of moisture from the warm Tsushima Current below.

Orographic lift: This moisture-laden air hits Japan's mountain spine and is forced upward. Rapid cooling at altitude produces extremely low-density snow — often just 3-5% water content, compared to 8-12% in the Alps or Rockies.

The result: "Japow" — arguably the lightest, driest powder snow on Earth. Niseko averages 14-18m of cumulative snowfall per season. Myoko Suginohara regularly exceeds 12m. No other developed ski region on the planet matches this consistency.

La Niña amplifies this: During La Niña winters, the Siberian High strengthens and shifts south, producing colder temperatures over the Sea of Japan. Warmer water + colder air = even more moisture pickup = even more snowfall. This is why ONI is the single strongest predictor of Japanese seasonal snowfall.

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