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Avalanche Forecast

Mar 23rd, 2015–Mar 24th, 2015
Alpine
3: Considerable
Treeline
2: Moderate
Below Treeline
1: Low
Alpine
3: Considerable
Treeline
2: Moderate
Below Treeline
1: Low
Alpine
3: Considerable
Treeline
3: Considerable
Below Treeline
1: Low

Regions: Sea To Sky.

The region remains in a lower probability/high consequence avalanche pattern with a snowpack structure that is atypical for this time of year. Conservative terrain selection remains critical.

Confidence

Fair

Weather Forecast

Monday Night: Convective precipitation amounts are hard to pin down. The region could see 10cm to as much as 25cm above 1000m with very little wind.Tuesday: Scattered convective flurries. Freezing level rising to 1500m in the late afternoon. Very little wind.Wednesday: Winds out of the SW begin to pick up as warm air floods into the region. Look for light SW winds at treeline, potentially strong SW winds at ridgetop. Freezing level should climb to 2000m by late afternoon. 2 to 4mm of rain possible.Thursday: 1 to 5mm of rain. Light SW winds at treeline, strong W/SW winds at ridgetop. Freezing level starting the day at 2000m, climbing to 3000m by the afternoon.

Avalanche Summary

Over the past week, isolated slab avalanches to size 2.5 have been running on the mid-March persistent weak layer. In a few cases, avalanches failed with light inputs such as remote triggers. Recent heavy snowfall and wind prior to the weekend resulted in widespread storm slab avalanche activity to size 2, but it has also added load to these deeper, more destructive layers. On Sunday, numerous large slab avalanches were observed in the Spearhead Range and on Ipsoot Mtn. The mid-March interface was the suspected culprit in most of these events. See this observation for a good visual: https://bit.ly/1CS2Nld https://bit.ly/1CS2Nld

Snowpack Summary

Deep and dense new storm slabs have formed in response to steady wind, snowfall and warm temperatures prior to the weekend. At lower elevations, rain has saturated the snowpack. Cornices may also be fragile. The mid-March persistent weakness has become a serious player. It consists of a variably reactive crust/facet interface that is buried about 100cm below the snow surface. The mid and lower snowpack are generally well-settled and strong.

Avalanche Problems

Persistent Slabs

The problem is such that some slopes are unlikely to be a problem, while others could produce large and destructive avalanches with potentially disastrous consequences. Additional snowfall Monday night may initiate a new round of large avalanches.
Avoid steep high consequence features, convexities and areas with a thin or variable snowpack.>Pay attention to overhead hazards.>Choose conservative lines and watch for clues of instability.>

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood: Possible

Expected Size: 3 - 5

Storm Slabs

New snow Monday night may create fresh storm slabs in high elevation terrain. Due to the convective nature of the system, "power flurries" may occur resulting in higher accumulations than anticipated.
Be alert to conditions that change with elevation.>The new snow will likely require a day to settle and stabilize.>

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood: Likely

Expected Size: 1 - 3