Loose Wet
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Yesterday, temperatures climbed well-above freezing at all mid and several upper-elevation weather stations. Field observations are limited, but we assume slopes receiving sustained sunshine experienced a Wet Loose avalanche cycle as last weekend's surface snow warmed. Slides were larger and more dangerous in the Flathead Range and southern Glacier Park, which benefited the most from the recent snowfall.
Temperatures this morning are warm, with readings on either side of freezing at mid and upper elevations. The overnight refreezing of the snow surface was poor, and we expect only a thin, unsupportable surface crust in many locations. As temperatures warm, this crust should break down quickly, allowing you to sink into the mushy snow beneath and increase the chance that you could trigger a wet loose slide. Resulting slides may travel far on the underlying crust and could trigger a larger slide on a buried weak layer. Upper-elevation locations exposed to south-southwest winds may remain frozen.
We are unsure if yesterday's warming affected shady aspects. Today's temperatures will top yesterday's and may affect snow in shady aspects. Slopes warming for the first time will develop rollerballs, which are a precursor to a wet slide. Choose lower-angle slopes where you or your machine sink more than a few inches into the surface mush—limit time spent in long-running gullies or above terrain traps where the snow can pile up deep.
(12/28/2022)
Dirty debris signifies that this slide ran on the ground removing the seasonal snow cover. This slide looks to be a wet loose. However, there may be a crown at the top of the slide.
Photo: Mark Dundas