Archived

Avalanche Forecast

Mar 15th, 2013–Mar 16th, 2013

Alpine

4: High

The avalanche danger rating in the alpine will be high

Treeline

3: Considerable

The avalanche danger rating at treeline will be considerable

Below Treeline

3: Considerable

The avalanche danger rating below treeline will be considerable

Alpine

3: Considerable

The avalanche danger rating in the alpine will be considerable

Treeline

3: Considerable

The avalanche danger rating at treeline will be considerable

Below Treeline

2: Moderate

The avalanche danger rating below treeline will be moderate

Alpine

3: Considerable

The avalanche danger rating in the alpine will be considerable

Treeline

2: Moderate

The avalanche danger rating at treeline will be moderate

Below Treeline

2: Moderate

The avalanche danger rating below treeline will be moderate

Regions: Cariboos.

Observations were limited on Friday and uncertainty exists with forecast freezing levels. Be alert to conditions that change with elevation and make observations continuously as you travel.

Confidence

Fair - Freezing levels are uncertain on Saturday

Weather Forecast

Saturday: Light snowfall becoming moderate overnight / Moderate to strong west winds / Freezing level at 1200mSunday: Light snowfall / Light to moderate northwest winds / Freezing level at surfaceMonday: Light snowfall / Light southwest winds / Freezing level at 900m

Avalanche Summary

On Thursday there was a widespread natural avalanche cycle which included several size 3 slabs. Some released to ground below 1500m where the snowpack had become saturated.

Snowpack Summary

Strong southwest winds, heavy snowfall, and warm temperatures in recent days have formed deep and cohesive storm slabs at treeline and above. Widespread cornice development has also taken place. At lower elevations rain has continued to penetrate the snowpack, and below 1400m the snowpack is reported to be isothermal. The recent storm snow overlies a weak layer of surface hoar or a sun crust that were buried on March 10th. Some areas had strong winds before the surface hoar was buried, so its distribution may be specific to sheltered and shaded terrain features. There is still concern for the buried layer of surface hoar from February 12th that is now down more than 1.5m in most places. Although less likely, the new load of snow and wind may overload this deeply buried weak layer in isolated terrain.

Avalanche Problems

Storm Slabs

Touchy storm slab conditions will continue in the wake of heavy precipitation and strong wind, especially in wind-affected terrain or in areas where recently buried surface hoar exists.

Choose conservative lines and watch for clues of instability.>Avoid exposure to cornices and overhead avalanche terrain, as large avalanches may reach the end of runout zones.>Stay off recent wind loaded areas until the slope has had a chance to stabilize.>

Aspects: All aspects.

Elevations: All elevations.

Likelihood: Likely

Expected Size: 1 - 6

Persistent Slabs

A layer of surface hoar buried on February 12th would now require a large trigger such as a large cornice fall, or an avalanche in motion. Although unlikely, the resulting avalanche would be very large.

Be aware of the potential for large, deep avalanches due to the presence of buried surface hoar.>

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

Elevations: Alpine, Treeline.

Likelihood: Unlikely

Expected Size: 3 - 7