Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Regions
Glacier.
Weather Forecast
The ridge of high pressure will mean another mostly sunny day today, with an alpine inversion. Expect a high of -1 with moderate SW winds at ridgetop. Overnight, a cold front will approach from the coast. Thrusday will be cloudy with flurries. Temps will range from -10 to -5 with gusty westerly winds. Friday will be mostly cloudy with flurries.
Snowpack Summary
Above 1700m 5-15cm of light snow sits on the Feb 14 crust, which is supportive to ~1900m. The Jan 30 crust layer is down ~1-1.25m is becoming more stubborn to trigger. Jan 15 surface hoar down ~1-1.5m gives sudden test results in isolated areas. The mid and lower snowpack is well settled. Nov 9 basal crust layer still present in the alpine.
Avalanche Summary
Solar triggered avalanches have been observed for the past 2 days to size 2.5. On the weekend, impressive deep slab avalanches occurred. A size 3.5 from the col between Clarke Peak and Mt Swanzy was likely triggered by cornice fall and ran on glacier ice. In the Asulkan Valley, a size 3.0 from Mt Pollux ran on the Nov 9 crust/to ground.
Confidence
Problems
Cornices
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.