Avalanche Forecast
Issued: Jan 25th, 2018 5:14PM
The alpine rating is Wind Slabs and Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Moderate - Due to the number of field observations
Weather Forecast
TONIGHT: Mostly clear. Ridge wind strong, southwest. Temperature -10. Freezing level lowering to valley bottom.FRIDAY: Mix of sun and cloud, light flurries. Accumulation trace. Ridge wind moderate to strong, west. Temperature -5. Freezing level valley bottom.SATURDAY: Cloudy, flurries. Accumulation up to 2 cm. Ridge wind light, south. Temperature -5. Freezing level valley bottom.SUNDAY: Cloudy, flurries. Accumulation up to 2 cm. Ridge wind moderate, southwest. Temperature -4. Freezing level 500 m.
Avalanche Summary
On Thursday explosive control work in the Castle area triggered a Size 3 avalanche from a shallow area that propagated and failed on the late-November layer deep in the snowpack. While in the Bull River area a natural Size 2 was observed on west-facing cutblock at 1600 m.The lack of activity can most likely be attributed to a lack of observations rather than snowpack conditions. The snowpack in the region remains suspect with several buried weak layers displaying classic signs of instability such as whumpfing and cracking.A recent video posted to the Avalanche Canada South Rockies field team Facebook page paints a pretty clear picture https://www.facebook.com/avcansouthrockies/videos/1894352117306941/.
Snowpack Summary
Up to 30 cm of recent storm snow now covers both a new layer of feathery surface hoar in sheltered areas as well as sun crust on solar aspects buried mid-January, and about 30-50 cm below the surfaces lies the early-January surface hoar layer.About 60-80 cm below the surface a weak layer of feathery surface hoar crystals and/or sun crust buried mid-December is found at treeline and below treeline elevations. Near the base of the snowpack the weak early-season layer of rain crust and sugary facets buried late-November exists. Although the snowpack structure is variable across the region, these persistent weak layers are generally widespread. Snowpack depths are also variable across the region and typically thinner in northern areas than in areas to the south.
Problems
Wind Slabs
Aspects: North, North East, East, South East, South.
Elevations: All elevations.
Likelihood
Expected Size
Persistent Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Valid until: Jan 26th, 2018 2:00PM