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Avalanche Forecast

Archived

Mar 5th, 2015–Mar 8th, 2015

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

Regions

Waterton Lakes.

Watch for weakening of surface layers and overhead cornices this weekend with solar warming and temperatures rising to just above freezing at mid elevation. Some good turns can still be found in sheltered, more northerly slopes below treeline.

Weather Forecast

Weekend temperatures will rise to just above freezing at mid elevation during mid day. Combined with solar influences watch for weakening of near surface layers and ridge line cornices. No new snow is forecast. Expect moderate westerly winds.

Snowpack Summary

Hard slabs are now found in all open areas at treeline and above. They overlie a layer of low density snow on top of strong temperature or sun crusts or old wind slabs.  Deeper persistent instabilities are presently bridged by a strong mid-pack in most locations. Watch for shallow higher elevation areas where triggering is still a possibility.

Avalanche Summary

March 4 saw a small cycle of natural avalanches failing on the previous crusts down 20 to 40cm as the snow from earlier in the week was redistributed on to northerly lee areas. No avalanches were observed on Thursday, March 5th

Confidence

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.