snownow

Every weather model, at your elevation.

Map

1 Location

2 Choose your adventure

3 Elevation

2,000 m

3 Forecast

Mountains › Japan

Ōnogara Dake snow forecast and mountain weather

Ōnogara Dake rises to 1,236 m in Japan. The forecast below starts at the summit; lower the height to see the slopes and valleys, or compare every model.

Ōnogara Dake snow forecast, day by day

DaySummit1,236 m500 m lower740 m1,000 m lower240 mFreezing level
Wed 28 Oct–––2,350–3,250 m
Thu 29 Oct–––3,100–3,550 m
Fri 30 Oct–––2,650–3,450 m
Sat 31 Oct–––2,400–3,350 m
Sun 1 Nov–––3,000–3,700 m
Mon 2 Nov–––2,550–3,700 m
Tue 3 Nov–––2,550–3,400 m
Total–––

Forecast snowfall worked out for each height from ECMWF (days in UTC, updated 6 hours ago). Not a measured snow depth. The forecast above has the hour-by-hour detail, wind and temperature, and every other model.

Mountains near Ōnogara Dake

More: Mountains in Japan · Mountains in Asia · The world’s highest mountains · Ski resorts

Questions about Ōnogara Dake

Will it snow on Ōnogara Dake this week?
Little or no new snow is forecast on Ōnogara Dake over the next 7 days (no new snow at the summit). Forecasts change, so check again closer to the time.
What is the freezing level on Ōnogara Dake?
Over the next 7 days the freezing level is forecast between about 2,350 m and 3,700 m. The summit is 1,236 m, so it stays above freezing even at the summit: rain is likely if anything falls.
How high is Ōnogara Dake?
Ōnogara Dake is 1,236 m (4,055 ft) high, in Japan.

Mountain heights and names: Wikidata (CC0).

Weather data by Open-Meteo.com (CC BY 4.0) from ECMWF, NOAA, DWD, Météo-France, MeteoSwiss, GeoSphere Austria, UK Met Office, ECCC, JMA and others. Terrain: Mapzen / AWS Terrain Tiles. Map: OpenTopoMap, © OpenStreetMap contributors. Ski runs and resorts: OpenSkiMap (© OpenStreetMap contributors, ODbL). Radar: RainViewer. Weather stations: Meteostat. Webcams: Windy. Place search: Open-Meteo and Photon (© OpenStreetMap contributors). Snow totals are worked out for your chosen height: each model’s precipitation × the share falling as snow there (from its freezing level and temperature) × the snow-to-water ratio. A model’s own snowfall is for its smoothed ground height, which can be far below the peaks, so ours can differ from it. Always check your local avalanche bulletin.