Dangerous conditions are expected this weekend. New snow and warming will contribute to the storm slab, cornice, and deep slab problems.
Avalanche problems
Cornices
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible - Likely
Size
1–3
Cornices are huge and are ripe for triggering. To avoid a nasty ride, give these monsters a wide berth when traveling along ridge crests.
Storm Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Likely
Size
1–3
Fresh storm slabs formed on Friday and will remain reactive to human triggers throughout the weekend. They'll be extra touchy in wind-exposed terrain.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Unlikely - Possible
Size
2–4
Once or twice a week we get a report of a large naturally-triggered deep persistent avalanche. Likely triggers for these destructive avalanches include storm loading, cornice falls or solar radiation, all of which are expected over the next few days.
Confidence
Moderate - Timing, track, or intensity of incoming weather system is uncertain
Weather Forecast
SATURDAY: Clear skies in the morning with increased cloud in the afternoon and light flurries, 30-50 km/h southwest winds, alpine temperature around -6 C.SUNDAY: Overnight snowfall of 10-15 cm easing off throughout the day, 30-40 km/h southwest winds, alpine temperatures around -4 CMONDAY: Cloudy with sunny breaks, 40-60 km/h southwest winds, freezing level spiking to 1800 m.
Avalanche Summary
A natural storm slab avalanche cycle occurred on Friday, mostly in the size 2-2.5 range. Storm snow was also reactive to skiers, producing several size 1-2 avalanches on a variety of terrain. Cornices are large and remain easy to trigger. A great image from Sunday illustrates just how surprising the results can be. Click here for details. A size 3.5 deep persistent slab avalanche likely occurred on Wednesday a northeast facing alpine slope on Mt Hosmer. It's thought to have been cornice-triggered and ran a distance of about 900m. This event highlights the isolated, yet destructive, nature of the deep persistent avalanche problem which should become more prevalent as we head into spring.Storm slabs will remain primed for human triggering on the weekend, while the warming trend will increase the likelihood of cornice failures and deep slab releases.
Snowpack Summary
Friday's storm delivered about 25 cm of heavy snow that settled into a touchy slab thanks to mild temperatures and moderate winds. The overall storm total since the start of the month now stands at roughly 70-120 cm. At times, strong southwest winds have extensively redistributed the snow forming large brittle cornices. An interface consisting of surface hoar, facets, stiff wind slabs, sun crusts, and a rain crust below 1900 m was buried in the middle of February. Little is known about the reactivity of this interface, but it may have the potential for large and destructive avalanches. Isolated basal facets still exist in shallow snowpack areas and can produce destructive full-depth avalanches. Likely triggers include intense storm loading, a cornice fall, or strong solar radiation.