Warm temps and poor overnight freezes are causing what will likely be the last major avalanche cycle of the season. Start early and be done early and be thinking about aspect and time of day. Good Climbing right now!!!
Weather Forecast
Sunday will be much like Saturday! Clear skies, warm temps and light winds out of the SW. Freezing levels will be around 2600m again so pay close attention to the quality of the overnight freeze. Avalanche danger will trend again from Mod/Low in the cool times of the day to HIGH in the heat of the day. START EARLY and dont be near anywhere south facing or under anything south facing later in the day.
Avalanche Summary
Numerous loose wet avalanches on all aspects except including pure north alpine. A few other deep persistent avalanches up to sz 3 were also noted fail on ground. Some are running full path taking out mature timber at the end of the runouts.
Snowpack Summary
Widespread crusts can be found on all aspects except for true north above 2400m. These crusts on south aspects are up to 20cm thick and fully supportive. As temperatures warm up during the day, these crusts are breaking down, loose wet avalanches begin to occur and as the heat penetrates deeper into the snowpack, deep slab avalanches become likely. There is a brief window between the two wherein there is good corn snow skiing but your timing has ton be bang on. Lower elevations are turning into a full on isothermal snowpack.
Problems
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.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.
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.