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Mountains › India

Deo Tibba snow forecast and mountain weather

Deo Tibba rises to 6,001 m in India, in the Pir Panjal (Himalayas). The forecast below starts at the summit; lower the height to see the slopes and valleys, or compare every model.

Deo Tibba snow forecast, day by day

DaySummit6,001 m500 m lower5,500 m1,000 m lower5,000 mFreezing level
Sun 25 Oct–––1,350–3,550 m
Mon 26 Oct–––1,300–3,750 m
Tue 27 Oct1 cm1 cm1 cm1,600–3,850 m
Wed 28 Oct–––1,600–3,950 m
Thu 29 Oct–––1,750–3,950 m
Fri 30 Oct1 cm1 cm1 cm1,850–4,050 m
Sat 31 Oct–––1,900–4,050 m
Total1 cm1 cm1 cm

Forecast snowfall worked out for each height from ECMWF (days in UTC, updated 7 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 Deo Tibba

More: Mountains in the Himalayas · Mountains in India · Mountains in Asia · The world’s highest mountains · Ski resorts

Questions about Deo Tibba

Will it snow on Deo Tibba this week?
Yes. About 1.2 cm of snow is forecast at the summit of Deo Tibba (6,001 m) over the next 7 days, most of it on Tuesday.
What is the freezing level on Deo Tibba?
Over the next 7 days the freezing level is forecast between about 1,300 m and 4,050 m. The summit is 6,001 m, so it should stay below freezing at the top all week.
How high is Deo Tibba?
Deo Tibba is 6,001 m (19,688 ft) high, in India.
Which mountain range is Deo Tibba in?
Deo Tibba is in the Pir Panjal, part of the Himalayas.

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.