We have a very complicated snowpack that will require a careful and conservative assessment before committing to any avalanche terrain. Ice climbs with significant overhead hazard should be avoided until the hazard abates.
Avalanche problems
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Likely
Size
1.5–3
Moderate winds, perfect for slab production has been observed at all elevations. Noticeably sensitive lee areas observed on NE, alpine aspects.
Storm Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Likely
Size
1–2.5
The new snow will continue to settle over time. Determining the strength of bond at the Dec. 11 interface will be key to safe travel in open features at treeline and below.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible
Size
2–3.5
Normally found 20-30cm off the ground. Potential for step-down avalanches if you trigger a wind slab or storm slab.
60cm of new snow has fallen since Dec. 11th in the Icefields, south to Rampart Creek areas (much less to the north), and has been redistributed by moderate SW wind. The resulting storm and wind slabs overly several weak interfaces - facets, crusts and isolated surface hoar. A deep persistent weaknesses still lingers in the bottom of the snowpack.
Avalanche Summary
A natural avalanche cycle triggered by this weeks storm resulted in numerous storm and wind slab avalanches up to size 3.5. Avalanche control work in the Parkers ridge area on Friday (Dec. 14th) produced numerous slab avalanches up to size 2.5 - direct evidence that despite natural triggering having slowed, human triggering remains likely.