The heaviest snowfall will likely be confined to the coast with the approaching system. The avalanche danger could be slightly lower in areas that receive less than 20 cm of new snow through Sunday.
Avalanche problems
Cornices
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible
Size
2–5
Cornices have grown large and weak and may pop off with continued growth or during periods of mild sunny weather.
Storm Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Likely - Very Likely
Size
1–5
It may be possible to trigger deep storm slabs in any terrain over 35 degrees, and particularly exposed lee terrain and cross-loaded gully features where wind slabs have formed.
Confidence
Fair - Intensity of incoming weather is uncertain on Tuesday
Weather Forecast
Synopsis: The active weather pattern continues into next week with a series of frontal systems affecting the region with short breaks in between each pulse.Overnight and Sunday: The first system arrives late Saturday bringing 10-15 cm overnight, and an additional 10-15 cm on Monday morning. The freezing level is around 600 m and winds are strong from the southwest. Monday: Cloudy with sunny breaks. The freezing level is near valley bottom and winds ease to light from the northwest. Tuesday: The next system arrives bringing 5-10 cm of snow and increasing winds.
Avalanche Summary
Several natural slab and loose wet avalanches up to size 2 were reported on Friday. There was also a report of a couple intentionally triggered slab avalanches up to size 2 that were 80 cm deep. Observations are generally limited to below treeline due to poor weather.
Snowpack Summary
Up to 100 cm of storm snow has fallen over the past few days. The new snow was reported to be dry and low density with no notable weaknesses. Deep and dense wind slabs have likely formed in exposed lee terrain and cross-loaded gullies. This new snow fell on a crust, old wind slab, and/or surface hoar depending on aspect and elevation. Most areas are reporting that the snow has bonded well to the underlying melt-freeze crust. Cornices that now loom over many features may become weak with continued growth and/or daytime warming. The mid and lower snowpack layers are generally well settled and strong.