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Avalanche Forecast

Archived

Jan 24th, 2025–Jan 25th, 2025

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Glacier.

5-10 cms of new snow with wind has created new windslabs. Expect these to be reactive, especially around ridgetop.

Cold temperatures can turn a minor incident into a serious one. Be sure to pack extra layers, a hot drink and emergency blanket or tarp.

Confidence

High

Avalanche Summary

Field teams observed skier triggered size 1's in the Connaught valley today, these were isolated to the new snow on old firm bed surfaces.

An avalanche cycle was observed in the park on Wednesday. The avalanches were in the 1.5-2 range and all looked to be the result of wind loading. Recent MIN reports also describe a reactive windslab problem.

Snowpack Summary

Moderate SW winds created variable, reactive surface wind slabs. Localised downflowing valley winds have created wind effect in open areas BTL. Sheltered areas have ~15cm of cold, faceted snow atop a denser, wind-pressed layer. Below this lies a weak interface (Jan 7th layer) down 30-60cm, comprised of surface hoar (all aspects) and or a thin crust on steep S aspects.

Weather Summary

High pressure settles in over the region giving clear skies and no significant snowfall.

Tonight Cloudy with clear periods. Ridge wind NW 10-25 km/h. Alp low -14C°. Freezing level (FZL) at valley bottom(VB)

Sat Mix of sun & cloud. Precip: Nil. Alp high -10C°. Ridge wind light. FZL at VB

Sun Sun & cloud. Precip: nil. Alpine high -2C°. Ridge wind NW 10km/h.

Mon Sun & cloud. Precip: nil. Alp high 0 C°. Ridge wind: NW 10 km/hr

Sunday

Terrain and Travel Advice

  • Be especially cautious as you transition into wind-affected terrain.
  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks, or recent avalanches.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.