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Avalanche Forecast

Archived

Dec 20th, 2018–Dec 21st, 2018

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

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Several large and destructive avalanches have occurred recently in this zone. Avoiding where avalanches start, run and stop remains the best course of action while we gather more information about the persistent weak layer across this zone. Be aware of your overhead exposure to large avalanche paths even at lower elevations.

Discussion

Avalanche Summary

Several large and very large natural, skier, and explosive triggered avalanches occurred in the Crystal area Monday through Wednesday. Many of these avalanches acted in surprising ways including wrapping around terrain features, running to the end of the runouts, and responding to relatively small triggers. Unusual avalanches such as these should cause us to step back and take notice. Recent avalanches are the simplest sign of avalanche danger. 

Thursday’s storm brought rain and high winds to West Slopes South, limiting the amount of new information. It’s important to note that we have far less recent information about the persistent weak layer distribution and sensitivity in the Paradise, White Pass and Chinook Pass areas. Assume a higher level of uncertainty if visiting other locales in this zone. 

On Tuesday a very large avalanche was triggered by a single small explosive at Crystal Mountain Ski Resort. This avalanche failed on the buried persistent layer, took out several adjacent avalanche paths, and ran full track to the valley. A ski patroller was caught, carried, and deployed his airbag. He survived with minor injuries despite the huge size of the avalanche.

Avalanche Details: NE aspect, 6600’, SS-AE-R4-D4-O 

Snowpack Discussion

Regional Synopsis: December 19, 2018

Why has the avalanche danger been so high for so long? Two reasons: A very active and wet weather pattern combined with a widespread persistent weak layer.

For perspective, the approximate snow totals from 12/9-12/19 are:

  • Mt Baker: 102”

  • Washington Pass: 55”

  • Stevens Pass: 76” mid-mountain

  • Snoqualmie Pass: 68” mid-mountain

  • Crystal Mountain 70” Green Valley

  • Paradise: 78”

  • Mt Hood Meadows: 44” mid-mountain

  • Olympics: 48”

In many areas, a layer of buried surface hoar and/or weak sugary facets was buried on December 9th. This layer has been the cause of numerous natural, explosive, and skier triggered avalanches. As this layer gets deeper it gets harder to assess. In short, the scenario is tricky and getting more dangerous by the day.

Higher snowfall totals along the Hwy 542 corridor/Mt Baker area have driven several avalanche cycles during this period. Loading from recent storms has been more incremental to the east and south of the Mt. Baker area, so we have not yet experienced a widespread cycle in other areas.

When will we reach the breaking point? It’s hard to say. What we do know is we have a deep weak layer, reports of very large explosives triggered slides at Mission Ridge and Crystal Mountain, and more storms on the way.

Be patient and continue to stick to lower angle slopes with nothing above you.  This is a good time to avoid areas where avalanches can start, run, and stop.

We’d like to thank all of you who have sent NWAC your observations. If you are out in the mountains, let us know what you see.

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.

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.