Minimize overhead hazard while the snowpack reacts to the rising freezing levels.
Avalanche problems
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible - Likely
Size
1–2
Strong SW winds, and significant amounts of snow available for transport have created wind slab in lee features.
Cornices
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible
Size
1–3
Rising freezing levels could result in fresh cornices to fail triggering deep instabilities.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Unlikely - Possible
Size
1.5–4
Use caution in shallow snowpack areas where deep weakness might be more reactive to a human load. Build trust slowly in the new snowpack before committing to any large rideable slope.
Exposed terrain at TL and above have been hammered with wind. In sheltered terrain the snow surface is likely to change with warm temperatures. The upper half of the snowpack is settling into a uniform slab over deep persistent weakness' at the bottom of the snowpack. Use caution in shallow areas where these deep weakness might be more reactive.