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Avalanche Forecast

Archived

Mar 2nd, 2020–Mar 3rd, 2020

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

Regions

Northwest Inland.

New snow on Tuesday will stress several weak layers, creating dangerous avalanche conditions. The potential for large destructive avalanches needs to be accounted for in your travel plans.

Confidence

Moderate - Uncertainties in both the snowpack structure and the weather forecast limit our confidence.

Weather Forecast

A series of fronts hit the region Monday night, Tuesday night, and Thursday.

MONDAY NIGHT: Moderate intensity flurries with 5-15 cm of snow, strong to extreme wind from the west, freezing level drops from 1000 to 500 m.

TUESDAY: Periods of heavy snow with 10-15 cm of snow, strong southwest wind, freezing level around 700 m, alpine high temperatures around -6 C. 

WEDNESDAY: Another 5 cm of new snow by the morning and then mostly cloudy throughout the day, moderate southwest wind, alpine high temperatures around -6 C.

THURSDAY: Scattered flurries with 3-8 cm of new snow, strong south wind, alpine high temperatures around -3 C.

Avalanche Summary

Poor visibility since the arrival of stormy weather on Sunday has limited observations, however natural wind slab avalanches are likely occurring in alpine terrain. Over the past few days there have been reports of wind slab, persistent slab (failing on the February 19 surface hoar layer), and deep persistent slab (failing on basal facets) avalanches. This pattern highlights how the current stormy weather is aggravating multiple weak layers in the snowpack.

Some of the recent activity includes:

  • Sunday: A natural size 2 slab avalanche on a south-facing alpine slope.
  • Saturday: A skier triggered size 1 slab on a northeast facing slope at 1500 m, failing on the February 19th surface hoar. There was also a great MIN report from Ashman with photos of recent size 2 wind slab avalanches on south-facing slopes.
  • Friday: A natural cornice failure produced a size 3.5 deep persistent slab on a northeast facing feature at 1800. Human triggered wind slab avalanches up to 30 cm in depth were running on the February 19th surface hoar too.
  • Thursday: Natural avalanches to size 2 running on the February 19th surface hoar.

Snowpack Summary

Extreme wind from the southwest and northwest have hammered open terrain, scouring some slopes and forming hard wind deposits in other slopes. Another 15-30 cm of snow by Tuesday afternoon accompanied with strong wind will form more fresh wind slabs.

30 to 50+ cm of settled snow overlies the Feb 19 surface hoar in sheltered locations and a sun crust on solar aspects, with the deeper slabs being found in the north of the region. The surface hoar may be most sensitive to human triggering at treeline which is a bit different setup than we're used to.

There are few different persistent weak layers (PWL's) we're watching in the mid and lower snowpack. A patchy layer of small surface hoar crystals and a sun crust both from early February are now 40 to 100 cm deep. A couple of weak layers that formed in January are buried in proximity to one another 80-140 cm below the surface. Below that, an early season crust lurks at the base of the snowpack. Some large avalanches have been triggered on these layers, usually during periods of rapid loading by new snow or wind or from large loads such as collapsing cornices. We're now in another one of those periods that could wake up the deep slab problem.

Terrain and Travel

  • Minimize exposure during periods of heavy loading from new snow and wind.
  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Use careful route-finding and stick to moderate slope angles with low consequences.
  • The trees are not the safe-haven they normally are at this time. Terrain at treeline is primed for human triggered avalanches.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.