Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterJan 17th, 2021–Jan 18th, 2021
South Rockies.
Dig down and investigate deeper layers in the snowpack before committing to big lines.
SUNDAY NIGHT- Mostly cloudy / Moderate to strong west-northwest wind / Alpine high temperature near -5
MONDAY - Sun and cloud / Light northwest wind / Alpine high temperature near -6
TUESDAY - Cloudy with isolated flurries / Increasingly strong southwest wind / Alpine high temperature near -9
WEDNESDAY - Cloudy with sunny breaks / moderate to light west wind / alpine high temperature near -7
On Thursday, explosives triggered a size 2.5 wind slab avalanche, and one natural size 3 persistent slab avalanche, both occurred on southeast aspects in the alpine.
Additionally on Thursday, a size 3 persistent slab avalanche was reported on an east aspect at 2400 m in the neighboring Waterton National Park region.
On Wednesday, were several natural avalanches to size 2.5 were observed and explosives also triggered avalanches up to size 2.5.
And just over a week ago (Jan 14), a natural size 3 persistent slab avalanche was reported on a large south-facing alpine slope in the Crowsnest Pass area.
These recent avalanches are a prime example of the "low probability; high consequence" scenario that persistent slab problems often create.
Strong winds have polished and pressed snow into hard slabs and sastrugi and stripped windward slopes. A melt-freeze crust covers surfaces up to 1850 m.
The lower snowpack consists of decomposing crusts and weak, faceted snow. In the Elk Valley, a decomposing surface hoar layer can be found around one of these crusts 60-120 cm below the surface. Avalanche activity on these layers in the lower snowpack has been sporadic, mostly triggered by large loads such as a wind slab avalanche, or a cornice fall. These deeper weak layers are most likely to be human triggered on steep, rocky slopes with a shallow or thin to thick snowpack.