Avalanche Forecast

Issued: Dec 22nd, 2018 10:00AM

The alpine rating is high, the treeline rating is considerable, and the below treeline rating is considerable. Known problems include Storm Slabs and Persistent Slabs.

Northwest Avalanche Center NWAC, Northwest Avalanche Center

Very dangerous avalanche conditions exist. New snow and wind will stress an already weak and scary snowpack. Travel in avalanche terrain is not recommended.

Summary

Discussion

Snow and Avalanche Discussion

Reports of very large natural avalanches continue in the Washington Pass area (some could destroy a house). Many had very wide propagation (up to 1 mile wide) and ran far distances downslope. These avalanches continue to break near the ground where a weak layer was buried on December 9th. This layer has been identified as near-surface facets and/or surface hoar. It is even blended with basal facets and depth hoar in areas further east and at upper elevations. Heavy snowfall will test this layer again. The balance could be tipped, and another round of very large and destructive avalanches is possible. Give the snowpack time to adjust. Be very cautious if you decide to travel in the backcountry on Sunday.

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

Storm Slabs

An icon showing Storm Slabs

New snow accompanied by strong winds will create storm slabs at all elevations. The incoming snow may not bond well to the old snow surface. Be especially careful of leeward areas below ridges and cross-loaded slopes. Any triggered avalanche within new snow has the potential to break further down in the snowpack creating a much larger, wider, more dangerous avalanche. Watch for recent avalanches, shooting cracks, and collapses. Seek out low-angle supported terrain away from overhead hazard.

Release of a soft cohesive layer (a slab) of new snow that breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. Storm-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.

 

You can reduce your risk from Storm Slabs by waiting a day or two after a storm before venturing into steep terrain. Storm slabs are most dangerous on slopes with terrain traps, such as timber, gullies, over cliffs, or terrain features that make it difficult for a rider to escape off the side.

 

Storm slabs usually stabilize within a few days, and release at or below the trigger point. They exist throughout the terrain, and can be avoided by waiting for the storm snow to stabilize.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Very Likely

Expected Size

1 - 1

Persistent Slabs

An icon showing Persistent Slabs

These avalanches could break near the ground and act in surprising ways. You may be able to trigger them remotely, from low-angle terrain or adjacent slopes. You may see signs of instability such as recent avalanches, snowpack tests that show propagation, collapses, or cracks that travel away from where you impact the snow. Give yourself a wide safety buffer to address the uncertainty. This dangerous problem continues to deserve a high level of respect and caution.

Release of a cohesive layer of soft to hard 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 Slabs.

 

The best ways to manage the risk from Persistent Slabs is to make conservative terrain choices. They can be triggered by light loads and weeks after the last storm. The slabs often propagate in surprising and unpredictable ways. This makes this problem difficult to predict and manage and requires a wide safety buffer to handle the uncertainty.

 

This Persistent Slab was triggered remotely, failed on a layer of faceted snow in the middle of the snowpack, and crossed several terrain features.

Persistent slabs can be triggered by light loads and weeks after the last storm. You can trigger them remotely and they often propagate across and beyond terrain features that would otherwise confine wind and storm slabs. Give yourself a wide safety buffer to handle the uncertainty.

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Likely

Expected Size

2 - 2

Valid until: Dec 23rd, 2018 10:00AM