Unsettled, cooling weather is promoting a refrozen snowpack with lingering wind slabs in the alpine.
A wind slab problem exists where recent storm snow has been redistributed by wind, particularly on leeward slopes and in alpine terrain.
Numerous wet loose avalanches up to size 1.5 have been observed, primarily occurring in solar-affected storm snow sitting on top of a melt-freeze crust.
The snowpack consists of 15 - 30 cm of old storm snow that is now moist and beginning to refreeze, except on high north-facing slopes where it remains dry. This overlies a melt-freeze crust and a deeper snowpack that is slowly refreezing. The persistent January drought layer is buried 50–130 cm deep, and total snow depths at treeline range from 130–200 cm.
Unsettled weather the next few days with cooler temps and occasional flurries. Warming back up on Thursday. See photo for a more detailed 3-day forecast.
Check out the Mountain Weather Forecast for the most up to date information.
