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Avalanche Forecast

Archived

Feb 8th, 2023–Feb 9th, 2023

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Below Threshold.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Below Threshold.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Below Threshold.

Regions

Yukon, Tutshi, Wheaton, White Pass East, White Pass West.

Fingers crossed Thursday's wind isn't enough to transform the great powder riding in White Pass into a minefield of wind slabs. Keep those savvy, sheltered terrain options at the ready in case blowing snow tells you the inevitable has arrived early.

Confidence

Moderate

Avalanche Summary

With the field team back in White Pass we received preliminary observations on Tuesday of a small scale natural wind slab avalanche cycle as a result of recent snowfall meeting with elevated winds, most recently from the west. Slab formation and releases appear to have been limited to alpine terrain thus far. No new persistent slab avalanches have been reported yet.

New surface instabilities aside, a couple of large (size 2-3) persistent slab, human-triggered and natural avalanches were reported last week. These avalanches occurred near ridgetops in north-to-northeast alpine terrain. These avalanches have showed an impressive capability to propagate across large distances. Here is a link to the most recent human-triggered size 3 avalanche.

Looking forward, this persistent problem is expected to grow less likely to trigger but will produce large, destructive avalanches if it is triggered. This means it still needs to factor into terrain decisions.

If you are out in the backcountry please share your observations to the Mountain Information Network!

Snowpack Summary

Light flurries with little wind Thursday should bring us to about 30-40 cm of recent snow resting on a variety of wind-affected surfaces and crusts, small surface hoar in places in the alpine, and a widespread 5-10 cm melt-freeze crust below roughly 1700 m.

The bottom portion of our new snow saw some wind effect before being buried, especially from the west but mainly in the alpine. This means slabs at upper elevations may be obscured by more recent low density snow.

A persistent weak layer of surface hoar and/or facets our field team has been tracking is now about 100 cm deep and exists on north facing alpine features. This layer doesn't appear to have produced any recent avalanches in the region and has shifted toward more stubborn results or non-results in snowpack tests this week.

Weather Summary

Wednesday night

Some clearing before clouding over again in the morning. Light southwest winds shifting east and increasing.

Thursday

Increasing cloud and flurries bringing up to 5 cm of new snow over the day, increasing a bit overnight. Light east winds. Treeline high temperatures around -10.

Friday

Becoming mainly sunny before clouding over again in the afternoon. 5-10 cm of new snow from the overnight period. Winds ramping up to strong southwest. Treeline high temperatures around -9.

Saturday

Cloudy with scattered flurries continuing from overnight with less than 10 cm total of new snow by end of day. Strong southwest winds. Treeline high temperatures around -5.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Pay attention to the wind, once it starts to blow fresh sensitive wind slabs are likely to form.
  • Wind slabs are most reactive during their formation.
  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
  • Persistent slabs have potential to pull back to lower angle terrain.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.