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Avalanche Forecast

Archived

Feb 22nd, 2012–Feb 23rd, 2012

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

South Rockies.

Confidence

Fair - Forecast snowfall amounts are uncertain on Saturday

Weather Forecast

A ridge of high pressure is expected to move into the region overnight. Northwest winds are expected to continue to be gusty and strong in the alpine and at treeline on Thursday. Continued high pressure is forecast for Friday morning, before a low pressure system moves into the region from the Pacific in the afternoon. Southwest wind and moderate precipitation is forecast to begin in the late afternoon or early evening. Snow and wind should continue overnight and into Saturday. The freezing level is expected to drop down to near valley bottoms on Wednesday night, and then rise to about 1000 metres on Thursday.

Avalanche Summary

A remote-triggered size 2.5 avalanche was reported from the Northern Elk Valley at 2350 m on Tuesday. The crown was 60-70cm deep and the avalanche initiated in wind slab overlying surface hoar. Numerous avalanches sized 1.5 were reported on Sunday (and likely Monday, although we didn't hear about them) at all elevations and focussed predominantly on easterly aspects. Remote-triggering was reported, where the avalanche was triggered from up to 100 m from where it initiated.

Snowpack Summary

Gusty wind has transported snow into windslabs at all elevations. In southern and western parts of the region, 40-50 cm of recent snow sits of a highly reactive weak layer comprising surface hoar (most prevalent in the west of the region), sugary facets on shady northerly aspects and sun crusts on solar aspects. This interface has started to react to human-triggering. Certain features of the reactivity, such as remote triggering and the ability to initiate avalanches on relatively low angled terrain, point to this weak layer shaping up to be quite dangerous. In areas further north, less snow has fallen on this interface--in the northern Elk Valley for instance, only around 15-20 cm lies above this interface. In lower snow areas, avalanche activity will likely lag behind higher snow areas, except for areas which have seen significant wind transport. In general, the mid-pack is quite strong in most locations. However, lingering concern remains for basal facets, particularly in shallower snowpack areas with steep, rocky start zones.

Problems

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

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.