The main concern is the buried surface hoar, facet, crust combo layer found predominantly at tree line and sub alpine elevations 'Whumphing' is being reported from this persistent weak layer (PWL).
Avalanche problems
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Unlikely - Possible
Size
1–2
Recent southerly winds have created new windslabs. Caution is warranted with lee and crossloaded features.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible - Likely
Size
1–2
The interface between rapidly settling storm snow and the previous surface is characterized by crusts. facets and surface hoar. New slabs are touchy in specific terrain - particularly steep, lee aspects at treeline and sub alpine elevations.
Weather Forecast
Some snow showers (10cm) is forecast for the southern end of our forecasting area and is accompanied by light southerly winds. This should do little to change our present avalanche hazard.
Snowpack Summary
Recent snowfall overlies a surface hoar, surface facet and crust combo, found predominantly at tree line and sub alpine elevations A relatively hard mid-pack is providing bridging strength over the weak basal facet layer. Below tree line has a supportive (albeit shallow) mid-pack.
Avalanche Summary
Yesterday - there was no natural activity observed between Jasper and The Big Bend and only limited results with the Avalauncher at Parkers Ridge (tree line elevation).