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Wallowa Avalanche Center

Professional Observation

Basic Information

Observation Details

Observation Date:
February 26, 2021 - February 26, 2021
Submitted:
February 26, 2021
Observer:
WAC - Killian Sump
Zone or Region:
Southern Wallowas
Location:
East Fork Pine Creek, Norway Basin

Signs of Unstable Snow

Recent Avalanches? 
Yes
Cracking? 
Isolated
Collapsing? 
None Experienced
Natural avalanche reported, skier triggered storm slab observed.

Snow Stability

Stability Rating: 
Poor
Confidence in Rating: 
High
Stability Trend: 
Worsening

Bottom Line

Over Thursday night, the Southern Wallowas saw 1.5-2.5 ft of low density snow accumulation depending on elevation. This fell on top of 6-8 inches on light density powder, which is all sitting on top of a rain crust from Monday, Feb 22. I skied generally below 6,000 ft today, and observed no collapsing or shooting cracks, however a member in the party triggered a small, localized 12 in deep storm slab on a steep convexity/rollover in the trees. The new snow has not yet formed a consolidated slab, yet will still fail if it is steep enough. Winds were up today from the E thru NW on the north end of the compass, and I'd expect wind slab in places near and above treeline.

Advanced Information

Weather Summary

Cloud Cover:
Mostly Cloudy
Temperature:
20 degrees F
Wind:
Moderate , E

After a rain event on Monday, we've had small pulses of light snow 3" at a time, adding to 9" along with strong gusty wind from the NW. Thursday night we received 20-30" of new, light snow depending on the elevation. Today Friday, the upper elevations saw strong winds from the E through NW, loading leeward terrain at ridgetops.

Avalanche Observations

 #  Date Location Size Type Bed Sfc Depth Trigger Comments Photo
1 Past 24 hours N Headwall
NW 7,150
D1.5 SS I-New/Old Interface 2-3 ft N-Natural None
2 Today East Fork Pine
S 5800
D1 SS 1 ft AR-Snowboarder
u-Unintentional
cut steep rollover, no one injured None
1
None

The new snow, although light and not a cohesive slab yet, has not had enough time to bond to the old rain crust. The depth of these storm and wind slabs are going to change dramatically depending on where you are.

Snowpack Observations

In the Southern Wallowas, the 2/22 rain event was light, and is not a very stout crust in most places. During the rain event, we had no propagation during our ECT on a NW aspect near treeline, and the following cool down did good things for our overall pack stability, generally right side up structure. The image is from Monday 2/22 and currently has 2-3+ ft of new light snow on top. Watching the new snow settle over the coming days will be interesting, to see how the new load sets up, changes, and bonds to the old.

During rain event, ECTX

Avalanche Problems

Problem Location Distribution Sensitivity Size Comments
Storm Slab
Isolated
Specific
Widespread
Unreactive
Stubborn
Reactive
Touchy
D1
D1.5
D2
D2.5
D3
D3.5
D4
D4.5
D5
Layer Depth/Date: 2-3+ ft
Wind Slab
Isolated
Specific
Widespread
Unreactive
Stubborn
Reactive
Touchy
D1
D1.5
D2
D2.5
D3
D3.5
D4
D4.5
D5
Layer Depth/Date: 2.5-4 ft

Terrain Use

Stayed below treeline today to avoid the wind and stayed in assessment mindset throughout the day, pushing it here and there on lower consequence steeper pitches.

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