Avalanche forecast

Blues

Wallowa Avalanche Center
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Avalanche danger

Fri
Alpine
3 · Considerable
Treeline
3 · Considerable
Below
2 · Moderate
Out of date — this forecast expired 3 years ago. You’re viewing past conditions, not the current bulletin.

Highlights

The storm system today will drop up to 10" of new snow and the new load will create unstable storm slabs on slopes >35 degrees. In addition, increasing winds will drift the light-density new snow onto leeward terrain features and build reactive wind slabs 1-2' deep on N-E-S aspects near ridgeline and cross-load ribs and gullies mid-slope.   Avoid slopes >30 degrees with recent wind deposits and watch for loose dry avalanches on steep south-facing terrain.

Today's forecast is sponsored by CB Construction.  

Avalanche problems

  • Storm Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2

    Overnight the Blue Mountans received 2" of new snow and up to 10" are forecasted to come down today. This new snow will not bond well to the underlying old snow surface and will create unstable conditions on slopes > 30 degrees. The best strategy for the next few days is to avoid avalanche terrain - stay off and out from under slopes > 30 degrees.

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2

    The 6" to 10" of new snow that has been deposited since the weekend is very light density and will be easily transported by the wind today. Overnight the winds have shifted from the NW to the SW and are currently 8-12mph gusting upper teens at upper elevations. The backing winds have created a wider area of wind-affected snow and riders are likely to find 1-2' reactive wind slabs on steep (>35 degree) on N-E-S aspects near ridgeline and on cross-loaded terrain features mid-slope. Look for smooth rounded pillows below ridgeline and on the leeward side of ribs and gully features mid-slope. It is best for the next few days to avoid steep alpine terrain where reactive wind slabs may lurk.

  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Unlikely
    Size
    1–2

    Over the last few weeks the buried persistent weak layers in the upper and lower snowpack have been mostly unreactive to human-triggering and have been gaining strength. I want to stress that pesistent grain types still exist throughout our snowpack. In particular, we have several facet/crust combos in the upper snowpack (top 3 feet) that remain a concern. There are also still some pockets of preserved and buried surface hoar. As our favorite astrologist Carl Sagan said, "The absence of evidence is not the evidence of absence." Be sure to evaluate the snowpack on any slope >35 degrees for buried persistent weak layers. If you see poor structure in the upper snowpack - namely strong over weak - then be sure to test those suspect layers for reactivity. Also, it is good protocol to avoid possible trigger points in the terrain like convex slopes, unsupported slopes above and below cliff bands, slopes punctuated with rocks, and areas in the terrain where the snowpack is shallow, <4' deep.

Avalanche Discussion

Protected and Sheltered Slopes Below Treeline

The snow quality on more protected and sheltered terrain is incredible right now. The cold temperatures and constant scud storms have left up to a foot of lovely light density snow in the Blue Mountains. This is the place to find the best snow quality and stability. There really isn't a good reason to go above treeline - unless you like to punish yourself with variable and more unstable conditions.

Wind Slabs

While great conditions are to be had below treeline, the situation changes dramatically as you move to treeline and above.  The recent north winds and now SW winds are scouring the alpine and creating reactive wind slabs 1-2' thick on leeward terrain features. It is a good idea to avoid steep slopes (>35 degrees) in the alpine for the next few days.

Persistent Slabs

Over the last few weeks the buried persistent weak layers in the upper and lower snowpack have been mostly unreactive to human-triggering and have been gaining strength. I want to stress that pesistent grain types still exist throughout our snowpack. In particular, we have several facet/crust combos in the upper snowpack (top 3 feet) that remain a concern. There are also still some pockets of preserved and buried surface hoar. As our favorite astrologist Carl Sagan said, "The absence of evidence is not the evidence of absence." Be sure to evaluate the snowpack on any slope >35 degrees for buried persistent weak layers. If you see poor structure in the upper snowpack - namely strong over weak - then be sure to test those suspect layers for reactivity. Also, it is good protocol to avoid possible trigger points in the terrain like convex slopes, unsupported slopes above and below cliff bands, slopes punctuated with rocks, and areas in the terrain where the snowpack is shallow, <4' deep.

Loose Dry

We have 6-12" of super light snow that is not bonding well to any slope that has an old melt-freeze crust or wind scab. In particular, it will be good to avoid steep (>35 degree) south-facing terrain where triggering a point release or sluff may get that new snow moving quickly down the slope, taking you off your feet or sled, and pushing you into terrain traps or stationary obstacles.

Regions covered