Avoid placing yourself under any terrain with cornices overhead as several failures have occurred recently producing large avalanches.
Lawinenprobleme
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Hochgebirge
Waldgrenze
Unterhalb der Waldgrenze
Wahrscheinlichkeit
Possible
Größe
1–2.5
Winds have abated on all but the highest ridge tops where slabs will be at their most developed.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Hochgebirge
Waldgrenze
Unterhalb der Waldgrenze
Wahrscheinlichkeit
Possible - Likely
Größe
1–3
The new snow from last week is settling and the interface with the old snow surface, buried up to a meter deep, is strengthening. Large triggers such as cornices have produced several releases in the past 48hrs.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Hochgebirge
Waldgrenze
Unterhalb der Waldgrenze
Wahrscheinlichkeit
Unlikely - Possible
Größe
1.5–3
The base of the snowpack is weak and facetted. Likely trigger locations are around rocks, where cold air can penetrate to the base of the snowpack, and shallow snowpack locations.
Weather Forecast
Little change is expected in over the holidays, forecasted winds will remain light and variable as arctic air seeps into the region during the next few days. Temperatures will remain cool as the sun traverses low to the horizon with highs of -10C and overnight lows of -17C. A detailed mountain weather forecast is available from Avalanche Canada.
Snowpack Summary
Last weeks storm snow is providing support underfoot to mountain travelers. Snow conditions at treeline are variable from power, in sheltered areas, to slabs in exposed locations and near ridges. The Dec. 11th persistent weak layer is buried 50-100cm. The deep persistent weakness lingers near the ground in the depth hoar and facets.
Avalanche Summary
Several deep releases from the alpine and been observed in the Icefields area. These avalanches are up to size 3 and appear to have been triggered by cornice failures from South Easterly facing slopes. It is likely these occurred at the interface of last weeks snow and then stepped down to the deep persistent interface at the base of the snowpack.