Avalanche Forecast

Low - Uncertainty is due to the timing of the incoming weather system. Uncertainty is due to the fact that deep persistent slabs are particularly difficult to forecast.

Dramatic weather through the forecast period.

THURSDAY NIGHT: Freezing level around 2100 m, moderate to strong southwest wind, no precipitation expected.

FRIDAY: Scattered cloud cover in the early morning building to overcast in the afternoon, freezing level around 1900 m, moderate to strong southwest wind picking up in the late afternoon, 5 to 15 mm of precipitation expected in the late afternoon/early evening, falling as rain at lower elevation and snow up high.

SATURDAY: Overcast, freezing level returning to valley bottom just before dawn and then staying near valley bottom all day, light variable winds at lower elevations, strong southwest wind in the alpine, 10 to 25 cm of snow possible.

SUNDAY: Broken cloud cover, freezing level near valley bottom, light to moderate southwest wind, no significant precipitation expected.

No avalanches have been reported since last week, but there have been limited field observations. A few natural size 2 wind slabs have been reported on north and east aspects in the neighbouring Kananaskis region.

A very large (size 3) deep persistent slab avalanche was observed north of Sparwood last Friday on a steep southeast facing alpine slope. This follows a pattern of sporadic deep slab releases in the upper Elk Valley including this natural avalanche from Feb 11 and this sled triggered avalanche from Feb 9. These types of large avalanches will be most likely during periods of heavy loading or intense warming.

A storm passing through Tuesday night delivered 5-10 cm to the region with closer to 15-20 cm along the northern parts of the region near Kananaskis Country. This snow was accompanied by strong to extreme wind from the west and formed fresh wind slabs in exposed terrain. A crust can be found near the surface up to 2300 m on solar aspects and up to 1700 m on all other aspects.

A thick rain crust sits 40-80 cm below the surface and can be found up to 2100 m. Avalanche activity was last observed at the faceting interface between this crust and overlying snow on February 17. The mid-pack is well settled and strong, but the base of the snowpack contains basal facets that are most prominent in shallow rocky start zones.

• Choose gentle slopes without steep terrain above.
• Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
• Avoid exposure to overhead hazards when solar radiation is strong.
• Avoid shallow snowpack areas, rock outcroppings and steep convex terrain where triggering is most likely.