Conditions vary across the region. In some places, there is still a real possibility of triggering a surprisingly large avalanche.
Confidence
Fair - Timing or intensity of solar radiation is uncertain
Weather Forecast
Temperatures are very warm (freezing level peaking near 2800 m) on Thursday and Friday, before cooling on Saturday with the passage of a cold front. Light precipitation is expected on Friday, followed by 5-10 mm precipitation on Saturday. This tapers to flurries on Sunday. Winds are light to moderate SW, changing to NW on Saturday as the front passes through.
Avalanche Summary
Loose wet avalanches to size 2 were triggered naturally and by skiers on Wednesday. These occurred on steep faces that caught some sun and at low elevations where the snowpack is water-soaked. A size 2.5 persistent slab failed on a steep shallow rocky feature at 2500 m, approximately 1 m deep. Cornices also collapsed naturally and with explosives.
Snowpack Summary
Recent storm snow appears to be settling and bonding with warm temperatures. SW winds have created areas of wind slab on some alpine lee features. Keep your eyes open for cornices, which may be sensitive to collapsing with the warm temperatures. The late-Jan crust/surface hoar layer, buried up to a metre deep, remains a key concern. Triggering this could produce a surprisingly large avalanche. The mid-January surface hoar is typically down 80-120cm and is most likely to be triggered from thin or rocky snowpack areas; or perhaps with a cornice fall, or an avalanche stepping down. The mid-December weak layer is down over 120cm, but is generally considered unreactive.
Problems
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.
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.
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.