Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Near to above overnight freezing temperatures, decreasing NE winds, and warmer daytime temperatures today should all increase wet snow instabilities. Transitional and variable snow surface conditions exist on most aspects. Melt freeze crusts have started to form on some lower elevation southerly aspects, but at this point are not well developed or widespread. The strong sunshine will quickly melt through any surface crusts and expose more wet snow. Unstable wet snow could form earlier, involving deeper layers of the upper snowpack with the potential for larger wet loose avalanches today.
Roller balls, pinwheels, and sinking into boot-top deep wet snow can indicate that enough wet snow exists for wet loose avalanches to occur. When the snow starts to feel wet and mushy, it's time to switch to a different aspect where the snow remains colder or move to lower-angle slopes without steep sunny slopes above.
(3/17/2024)
A D1 wet loose avalanche was triggered at 10:30am. 8900'. South side of Round Top, Carson Pass.