I remotely triggered a large avalanche from a safe ridgeline above. I also found weak layers in the middle of the snowpack that produced unstable snowpack test scores.
Afternoon wx: there was a lull in the storm between around 1200 and 1500, with S-1 to S1 precip afterwards. Winds were light, but I could see active transport in the upper elevations of the Boulders and Smokys on my drive to the TH.
# | Date | Location | Size | Type | Bed Sfc | Depth | Trigger | Photos | Details |
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1 |
Dec 30, 2022 (Exact) |
Baker Ck - above Baker Lake S 9500ft |
D2 | HS-Hard Slab | O-Old Snow | 1.5ft |
AS-Skier r-Remote |
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I did not see any other avalanches, but the visibility was poor and I likely would not have seen anything in the adjacent terrain.
My primary goal was to look at weak layers on solars in the upper snowpack, and to look at the amount of snow and any avalanche activity in the area since 12/26.
I found 12cm of medium-density new snow in the Baker lot. Near Baker Lake, I found 40-45cm of snow on top of the 2-3cm thick Christmas heat-wave crust. This snow was well bonded to the crust, which was essentially just a rigid portion of the upper slab in the snowpack.
SE @ 8400' : 12/19 down 50cm, produced ECTP 15,18, 23 and ECTPV (broke as I was sawing the column, I unintentionally levered on the saw when finishing the cut). 11/27 down 100cm, produced ECTP 21, 22, 34 (non-hulk smash, just additional shoulder hits). FC/DH at base of the snowpack were moist and showing signs of healing, but the upper portion of this layer (11/27) was still dry with 2-3mm striated cups.
Problem | Location | Distribution | Sensitivity | Size | Comments |
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Layer Depth/Date: down 50-65cm Weak Layer(s): Dec 8, 2022 (FCsf) Dec 19, 2022 (FC) Comments: Rose shaded based on where I was looking at this layer today, it likely extends down into lower elevation terrain. It may still also be problematic where associated with SH, but observations on this are limited. |
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Layer Depth/Date: down 100cm Weak Layer(s): Nov 27, 2022 (FC) Comments: Slab over this layer varies considerably in thickness, particularly in wind affected areas. Sensitivity appears to be a function of burial depth. In places where it is buried more deeply, this layer is gradually improving. In places where it is closer to the surface it is lingering and not improving. |
I did not encounter wind slabs as a problem today, but visible transport in Boulders and Smokys and plenty of snow for transport leads me to suspect they are present in places.
I avoided large, steep, unsupported avalanche terrain and the runouts of large paths.