Avalanche Forecast
Issued: Jan 19th, 2023 4:00PM
The alpine rating is , the treeline rating is , and the below treeline rating is Known problems include Deep Persistent Slabs and Wind Slabs.
SH,
Avalanche Canada
Good skiing can be found on low-angled terrain above treeline. The snowpack remains generally shallow and weak, a little less so to the West. Do not lose sight of the unpredictable nature of the deep persistent slab problem even though conditions appear to have improved.
Summary
Confidence
Avalanche Summary
A few small surface avalanches triggered by explosives were reported by Lake Louise patrol today. No other avalanches observed or reported.
Snowpack Summary
Dribs and drabs of snow over the past 2 weeks have amounted to 10cm. This sits on a surface hoar /crust layer which is sporadic in the region. The Dec 17 surface hoar/sun crust layer is down 25-50cm, and generally not reactive. The Nov. 16 deep persistent layer is down 40-90cm and continues to produce sudden failures in snowpack tests. In Little Yoho, these two layers are deeper and more spread apart in the snowpack.
Weather Summary
30-50km/h westerly alpine winds overnight into Friday AM, then diminishing to 20-40km/h from the NW. Temperatures will remain at valley bottom with highs of -5C to -10C at ridgetop.
Terrain and Travel Advice
- Uncertainty is best managed through conservative terrain choices at this time.
Problems
Deep Persistent Slabs
The lower snowpack is comprised of weak facets and depth hoar with the upper snowpack forming a 40 to 90cm thick slab above. This weak basal layer is uniform across most of the forecasting region and has been responsible for most of the avalanche activity to date this season.
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Wind Slabs
It is forecast to be windy on Thursday night, which could blow the 10cm of low-density snow into wind slabs on lee aspects.
Aspects: North, North East, East, South East.
Elevations: Alpine.
Likelihood
Expected Size
Valid until: Jan 20th, 2023 4:00PM
