Lawinenlagebericht

Galena Summit & Eastern Mtns

Sawtooth Avalanche Center
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Lawinengefahr

Sat
Hochgebirge
2 · Mässig
Waldgrenze
1 · Gering
Unterhalb
1 · Gering
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Veraltet — dieser Lagebericht ist 4 years ago abgelaufen. Du siehst vergangene Verhältnisse, nicht den aktuellen Bericht.

Kernpunkte

Watch for pockets of wind-drifted snow in upper elevation and alpine terrain. Wet snow avalanches are possible if the sun stays out longer than expected this morning. If you're sinking into a mushy snowpack, stick to gentler slopes or find cooler snow to ride.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–1.5

    Wednesday, I observed a few small wind slabs in the central and southern Sawtooths. Some of these slabs occurred very near ridgelines and some released on aprons and below cliff bands where recent snow "spin-drifted" into thicker slabs. Much of the recent wind came from the S, SW, and W depositing small slabs on shadier aspects in the alpine. 

    Some slabs may have formed over weak snow that developed during the drought of January and early February. This slide (report) in the Smoky Mountains illustrates what's possible in isolated areas with ideal wind-loading and a well-preserved weak layer. This problem is not widespread, but worth keeping on your radar. 

    If the snow suddenly gets deeper and/or stiffer, you've found a wind slab. If you see cracks shooting out from your skis or boards, think about the consequences of being knocked over by a small avalanche before committing to skiing or riding the slope.  

    ADDITIONAL DISCUSSIONCloud cover and cooler air will reduce the chance of wet snow avalanches. That said, the snowpack will take a bit of time to solidify after days resembling a bowl of oatmeal. If the sun peaks through the clouds, it won't take long to break down any surface crusts that formed last night. If you're sinking into slush, find gentler terrain or cooler slopes to ride.

    (2/26/2022) Skiers in Pole Cr triggered these two very small wind slabs on Saturday, 2/26. Once initiated, it appears that they entrained weak, sugary snow that exists in the surface layers of the snowpack.

Avalanche Discussion

Weak snow developed at the surface during the drought of January and February. Small storms clipped the northern end of the forecast area, favoring the Banner Summit Zone. Tuesday's storm brought an additional 8-10" of dense snow to Banner Summit above about 8,000' capping off a slab that's anywhere from 1-1.5' thick. This last storm proved to be just enough to tip the scales, producing multiple slab avalanches near Bull Trout Point (observation). 

South of Banner is a different story. It's snowed less, and the slab is thinner. Only a handful of slab avalanches were observed in the Sawtooths, most of which were small wind slabs (photo). This doesn't mean the weak layer in these zones is absent. Wednesday in the northern Boulders, Chris found unstable snowpack test scores, and observed cracking in ~1' drifts (observation). These drifts sat on the similar weak layers that formed during the drought. The difference here, as well as other areas outside of Banner Summit, is that these conditions are more infrequent and require some wind-loading to build the slab. 

Wednesday, I spotted this large persistent slab avalanche on the N. face of Saviers Pk in the Smoky Mountains. While an apparent outlier, it's an indication that this problem lurks in isolated areas with ideal wind-loading and a well-preserved weak layer. You're not likely to find many locations that can produce this large of a slide, but the possibility is there. This avalanche and the ones near Banner Summit may foreshadow what's to come if large-scale snow returns to the forecast area.

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