We are expecting a significant rise in avalanche danger (if the forecasted snow fall actually arrives!). Very conservative route selection is in order.
Avalanche problems
Loose Dry
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Likely
Size
1–2
Sluffing is expected in steep terrain, potentially on all aspect Significant entrainment could occur given the weak nature of the existing snowpack.
Storm Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Likely
Size
2–3
Expected snowfalls of up to 20cm and strong SW winds will create storm slabs in lee and cross-loaded features. Given the weak layer that most of these slabs will lie on, avalanches could be easy to trigger.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible
Size
2–3
Deeply buried weak layers dominate the snowpack. Avalanches are more likely triggered from shallow snowpack areas and step down to the basal facets and involve the entire winters snowpack.
Confidence
Low - Intensity of incoming weather systems is uncertain
Weather Forecast
Wednesday will be warm and very windy with a mainly cloudy sky. The big unknown is the amount of snow fall. Some models are calling for almost no snow accumulation, while other models are predicting 15 to 20cm by Wednesday afternoon. Most models agree that Thursday and Friday will be cloudy with only light precipitation.
Avalanche Summary
Two naturally triggered size 2.0 slab avalanches were observed today. One occurred on a West aspect of Mt Engadine in an Alpine feature. The other avalanche occurred at Treeline on a steep North aspect. Both of these avalanches appeared to have failed on the basal facets and ranged between 60 an 80cm deep.
Snowpack Summary
Trace amounts of new snow have fallen in the past 24hrs and very light flurries were falling this afternoon. The snowpack is settling due to the recent warm temperatures. Surface snow was moist on solar aspects up to 2100m and this may extend higher in elevation (this is unconfirmed). Intense snow transport was observed at ridge crest and it is very likely that further wind slab development has occurred in the Alpine. The remainder of the snowpack remains weak and facetted, and it is likely that an avalanche initiating in the upper snowpack will steep down to the basal layers.