Loose Wet
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–1.5
This problem will be confined to very steep, sun-exposed slopes. Depending on location, surfaces of wind-packed snow or melt-freeze crusts may break down, allowing softer snow underneath to become entrained. Exercise caution near large rock outcrops and cliff bands, as these features can enhance the rate of surface heating.
As you travel, monitor for where snow surfaces are becoming wet and unconsolidated. Use boot penetration on representative aspects to gauge surface stability to your intended terrain. If you observe signs that the upper snowpack is losing strength, such as rollerballs, greasy snow atop a firm crust, or sinking into mushy snow past your ankles, seek mellower or shadier terrain.
With high clouds present overnight, the snowpack may not have experienced as strong a refreeze as temperatures might suggest, and softer-than-expected surfaces may be present. On the contrary, high clouds throughout today will limit the amount of solar input surfaces can receive and decrease the rate of softening. This weather factor holds inherent uncertainty on which way stability will trend, so come prepared to self-evaluate conditions.
Continue to give cornices a wide berth when traveling above or below them.
(4/4/2026)
This is a representative snow structure for many solar aspects near and above treeline. Recent storm snow above a firm and supportable crust. The top inch of surface snow contained meltwater. As water continues to weaken the underlying dry snow, the potential for wet loose avalanches exists.
Photo: Eric Falconer