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Mountains › Russia

Akademia Nauk snow forecast and mountain weather

Akademia Nauk rises to 1,180 m in Russia, in the Eastern Range. The forecast below starts at the summit; lower the height to see the slopes and valleys, or compare every model.

Akademia Nauk snow forecast, day by day

DaySummit1,180 m500 m lower680 mFreezing level
Mon 26 Oct––0–600 m
Tue 27 Oct––0–400 m
Wed 28 Oct5 cm5 cm0–250 m
Thu 29 Oct<1 cm<1 cm0–150 m
Fri 30 Oct––0–400 m
Sat 31 Oct40 cm30 cm200–1,200 m
Sun 1 Nov4 cm2 cm0–1,150 m
Total48 cm37 cm

Forecast snowfall worked out for each height from ECMWF (days in UTC, updated 1 second ago). Not a measured snow depth. The forecast above has the hour-by-hour detail, wind and temperature, and every other model.

Mountains near Akademia Nauk

More: Mountains in the Eastern Range · Mountains in Russia · Mountains in Asia · The world’s highest mountains · Ski resorts

Questions about Akademia Nauk

Will it snow on Akademia Nauk this week?
Yes. About 48 cm of snow is forecast at the summit of Akademia Nauk (1,180 m) over the next 7 days, most of it on Saturday.
What is the freezing level on Akademia Nauk?
Over the next 7 days the freezing level is forecast between about 0 m and 1,200 m. The summit is 1,180 m, so the summit will be below freezing at times and above it at others.
How high is Akademia Nauk?
Akademia Nauk is 1,180 m (3,871 ft) high, in Russia.
Which mountain range is Akademia Nauk in?
Akademia Nauk is in the Eastern Range.

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.