Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
As the sun emerges today and temperatures continue to rise, the potential for wet avalanches will increase throughout the day. When a snow-covered slope warms up and begins to melt, the bonds within the snowpack start to break down, leading to a rapid loss of cohesion and stability. This warming effect can make the snowpack more prone to sliding, especially on steep terrain. Visible signs such as rollerballs, pinwheeling, and punchy or unsupportive snow underfoot are strong indicators that the slope is warming and could be approaching a critical failure point.
Since this process is heavily influenced by both air temperature and direct solar radiation, you can use a slope’s aspect to make safer travel decisions. East- and south-facing slopes tend to warm up the fastest, receiving early and intense sun exposure. West-facing slopes, while slower to heat up, become increasingly suspect in the afternoon hours as the sun shifts. North-facing slopes typically stay cooler and retain shaded conditions for longer, making them generally more stable when wet avalanche danger is a concern.
Keep these patterns in mind as you move through the terrain. If you encounter a slope that has been exposed to sunlight for a prolonged period—especially one showing signs of instability—it’s best to avoid traveling on or directly beneath it. Choosing cooler, shaded aspects and moving efficiently through sun-exposed areas earlier in the day will help reduce your exposure to this warming hazard.
(4/4/2025)
Lots of rollerballing from today's warm-up. These were observed on east through south to west-facing slopes at mid and lower elevations. This is an early indicator that slopes are softening quickly and provoking a wet slide may be imminent. West Cabinet Mountains. April 4, 2025.
Photo: Chris Bilbrey