Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 2
The entire Wasatch Range is plagued with a poor snowpack of weak faceted snow and depth hoar. This avalanche problem - known as a persistent weak layer (PWL) - exists on mid and upper elevation slopes facing west, through north, and east. This weak snow can also be found on some upper elevation southeast aspects. And to keep us on our toes, many snow surfaces were covered with a 5mm layer or surface hoar on Thursday. One long-time avalanche professional described our current snowpack structure as an "unprecedented weakness." A touch hyperbolic? Perhaps. But our thin 1-3' deep snowpack contains some of the weakest snow many have ever seen this late into January.
Over this past week, this PWL problem has been moving to a period of dormancy, but it will quickly come to life as we place a new load of storm and/or wind-driven snow on top of it. To put things in perspective, during the entire week of Jan 1-7 the central Wasatch received about 12" of snow containing nearly 1" of water. During this time, over 20 human-triggered avalanches were reported to the UAC, almost all failing in the PWL. Since that first week in January, our snowpack has grown even weaker, and we are now talking about placing an even greater load in roughly a 24-hour period.
Danger Trend: Rising
Angular, faceted snow crystals. [Dave Ream photo]