Rapid loading or rapid heating will cause stability to deteriorate quickly. Pay lots of attention to the aspect you are traveling on.
Confidence
Fair - Timing, track, or intensity of incoming weather system is uncertain on Friday
Avalanche Summary
Sporadic natural avalanche activity up to sz 3 continues in all three elevation zones. The majority of these slides that are occurring are related to daytime heating.
Snowpack Summary
Spring conditions. The snowpack is settling rapidly. Surface crusts are melting during the day and re-freezing at night. The snowpack has gone isothermal at lower elevations on the warmer days. Even North aspects have been affected with moist snow as high as 2500m. Where cornices exist they are large and sagging.
Problems
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.
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.