Avalanche Forecast

Issued: Mar 13th, 2012 10:32AM

The alpine rating is high, the treeline rating is high, and the below treeline rating is considerable. Known problems include Wind Slabs, Persistent Slabs and Storm Slabs.

Avalanche Canada jfloyer, Avalanche Canada

Next storm is expected to arrive late on Wednesday. If you're sick of seeing red, read the forecaster blog.

Summary

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Wednesday: A Pacific Frontal system arriving in the afternoon will bring around 5-15cm new snow with continued strong SW winds. Freezing levels will be around 1000m. On Thursday, a stronger pulse of precipitation will bring 10-20cm new snow, again with strong SW winds. Freezing levels will go up to around 1500m, or even a little higher in the south of the region. On Friday, precipitation will continue but should become lighter. Freezing level again around 1500m.

Avalanche Summary

On Monday, several size 2-2.5 slabs released naturally (likely from wind-loading), which are suspected to have failed on the mid-February persistent weakness. A helicopter remotely triggered a size 1.5 slab, part of which stepped down to basal facets. A skier was also swept over a cliff in a size 1 slab which failed on the mid-Feb layer. On Sunday, a group of skiers triggered a size 3.5 slab 900m wide and 80-140cm deep on a north aspect in the southern Purcells. Late last week, large (size 2.5-3.5) human and explosive-triggered slabs were reported on all aspects, with crowns 40-120cm deep.

Snowpack Summary

80 to 160 cm storm snow now overlies the prominent surface hoar layer of mid-February. The storm snow is reacting readily to both natural and human triggers. The mid-February surface hoar layer is more stubborn and not reacting everywhere, but has regularly been producing large avalanches up to size 3.5, which indicates it is very much still alive and needs to be treated with the utmost respect. This layer is widespread, so defining safe zones based on elevation or aspect may not be the best idea right now. Of course, shallower snowpack areas are those where you are more likely to trigger it, as well as convex rolls, and rocky or uneven terrain features. If you know that a slope has already avalanched on that layer, it may be a better bet, although you still need to factor in the effect of recent storm snow amounts and whether reloading is an issue. Operators continue to monitor basal facets, especially in shallow, rocky areas, but with all the recent storm snow, the basal weakness has not been of undue concern recently.

Problems

Wind Slabs

An icon showing Wind Slabs
Mostly S and SW winds, however, recent reverse-loading has occurred in response to E winds. Expect wind slabs to be fat, touchy and windspread.

Aspects: North, North East, East, South East, South, South West.

Elevations: Alpine, Treeline.

Likelihood

Very Likely

Expected Size

1 - 5

Persistent Slabs

An icon showing Persistent Slabs
The deep nature of the mid-February surface hoar layer makes potential avalanches triggered on this layer large and destructive. Regular and ongoing avalanche activity associated with this layer indicates it is very much still alive.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Likely

Expected Size

4 - 8

Storm Slabs

An icon showing Storm Slabs
If forecast heavy amounts of new snow come through, storm slabs may overload buried weaknesses & could even step down, producing large avalanches.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Likely - Very Likely

Expected Size

2 - 6

Valid until: Mar 14th, 2012 9:00AM

Login