Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2–3
It's not over yet! 6500ft freezing levels and precipitation will continue through Friday, and very large avalanches will run. From our limited observations on Thursday we gathered that many large (D2) avalanches ran naturally in wet, heavy surface snow. The avalanches picked up a lot of mass as they traveled downhill, ending in several-foot-thick debris piles. Water will percolate further down into the snowpack, potentially causing larger and deeper avalanches on Friday. Since the initial wetting and natural avalanche cycle occurred Thursday, we don't think avalanches will occur quite as frequently on Friday as they did the previous day, despite possibly being larger.
Glide avalanches will probably be waking up on steep, smooth faces, in addition to concerns of large sagging cornices breaking. In below treeline areas, most snow surfaces were old melt forms that could withstand the rain, although towards the upper reaches of the BTL some low density snow was present. This would have been impacted by the rain and warming with natural avalanches Thursday. A human-triggered avalanche could still probably occur at lower elevations. Keep in mind that concerns remain regarding large and very large avalanches running from higher elevations down to lower elevations. Avoid traveling in avalanche terrain on Friday.
A large debris pile from a natural avalanche on Mt Herman which occurred during a storm on 1/12/21, exactly 2 years ago. These huge debris piles are probably very similar to ones that we'll see after this storm passes through: very large, and not something you'd want to get caught up in. Photo: Trevor Konstanich