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Avalanche Forecast

Archived

Nov 24th, 2015–Nov 25th, 2015

Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.

Regions

Northwest Inland.

The snowpack is extremely variable depending on aspect and elevation. Stiff wind slabs with wide propagations may be ripe for rider triggering. Check out the Mountain Information Network. Give info, get info!

Weather Forecast

The arctic high remains stationary over the north giving cool and dry conditions on Wednesday. Treeline temperatures will hover near -12 with light winds from the northerly quadrants. Late Wednesday, warm air aloft will start to invade the coastal regions allowing temperatures to rise anywhere from 0-5 degrees between 1100-2500 m. Ridgetop winds will also change, blowing light from the southwest well into the weekend.

Avalanche Summary

No new avalanches have been reported. Newly formed wind slabs may remain sensitive to human triggering for the next few days, especially in areas with buried persistent weak layers.

Snowpack Summary

The snowpack is extremely variable depending on aspect and elevation. I suspect new wind slabs developing on reverse loaded southerly slopes and widespread surface crusts at lower elevations. At upper elevations, last weekends storm likely produced stiff wind slabs on northerly aspects. The reactivity of these new wind slabs will likely change with elevation and underlying snowpack structure. Due to limited observations, I have very little confidence in what that underlying structure may be, although I suspect faceting, crusts and surface hoar may exist. However; how are they adjusting and reacting as shears? Are they visually distinct and reacting like a cash register when tested? Or are they becoming hard to find with a more resistant shear characteristic? If I were traveling in the mountains, I'd maintain an investigative approach and dig down to test for weak layers before committing to a slope.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.