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Archived

Avalanche Forecast

Dec 18th, 2018–Dec 19th, 2018
Alpine
4: High
The avalanche danger rating in the alpine will be high
Treeline
4: High
The avalanche danger rating at treeline will be high
Below Treeline
4: High
The avalanche danger rating below treeline will be high
Alpine
4: High
The avalanche danger rating in the alpine will be high
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
3: Considerable
The avalanche danger rating below treeline will be considerable

Regions: Mt Hood.

Very dangerous avalanche conditions exist! Natural avalanches and human-triggered avalanches will be life-threatening on Tuesday.

Discussion

UPDATE: AVALANCHE WARNING IN EFFECT as of 0730 on 12/18/2018

Very dangerous avalanche conditions exist at all elevations and these conditions have been confirmed by Mt. Hood Pro Patrol on Tuesday morning. Avalanches are near certain on Tuesday. Over 2" of precipitable water fell overnight, with an additional 2" of loading on Tuesday.

Weak snow formed and buried earlier in the month can still be found in the upper snowpack. On Monday, Mt. Hood Meadows pro-patrol found buried surface hoar most intact in sheltered locations from 5500 to 6500 ft with the surface hoar layer below 5500 ft. While this layer was preserved intact 16-20" below the snow surface, it was neither reactive in snowpack tests nor involved in any recent avalanche activity. Several rain crusts were found above this layer. We will continue to track this layer and there is a small chance that with loading or rain it could produce a wet slab.

Snowpack Discussion

Updated Regional Synopsis 20181216

Dangerous and fickle avalanche conditions remain as active weather continues into the week. Thick slabs of new snow (2-5 feet) are perched above a weak layer of faceted crystals. Avalanches triggered on this layer could be very large and life threatening.

Reports continue to come in of very large natural and triggered avalanches in the northern and eastern zones. For perspective, several of these slides have been classified as D3, or large enough to destroy a house. You can find similar snowpack structure responsible for these avalanches in many other locations throughout the Cascades, including Stevens and Snoqualmie Passes.

Anyone accessing alpine areas should limit their exposure to areas where avalanches start, run and stop. In some places the weak snow will talk to you by whumpfing and cracking. In other places, the heavy blanket of new snow is thick enough that it can give a false sense of stability while it masks the dangerous layering below.

Approximate snow totals from 12/10 - 12/16:  

  • Mt. Baker: 75”

  • Washington Pass: 35”

  • Stevens Pass: 42”

  • Snoqualmie Pass: 36”

  • Paradise: 51”

  • Crystal Mt Base: 29”

  • Mt. Hood Meadows: 21”

  • Olympics: mix of rain and snow, no net gain

The change in the snowpack is pretty dramatic with elevation. Height of snow decreases rapidly below 4500’ at Baker and Washington Pass, 5500’ at Crystal/Rainier. The Passes have better low elevation coverage, but it's still pretty thin below 4000’. With additional warm storms in the forecast, this pattern is expected to continue for awhile. Mt. Hood and Hurricane Ridge have low snow coverage below 5000’.

If you're out in the mountains, please let us know what you see.

Be cautious and get home safe.

Avalanche Problems

Storm Slabs

Mt. Hood Meadows Pro patrol identified wet snow over dry snow from 5200' up to over 6000' as rain falls on 12-15" of snow which fell overnight. Rain then saturated the upper 3-4" of snow, creating a denser wet slab on top of the dry snow. This slab broke easily on isolation of the columns. These storm slabs are almost certain to be triggered either naturally with additional loading or by human trigger and they will be large, potentially releasing within storm snow or on a buried weak layer previously identified.   

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: Certain

Expected Size: 1 - 1

Wind Slabs

Strong winds have created very large wind slabs that are unevenly distributed and are likely to be sensitive to human trigger.

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.

 

Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas..

 

Wind Slab avalanche. Winds blew from left to right. The area above the ridge has been scoured, and the snow drifted into a wind slab on the slope below.

 

Wind slabs can take up to a week to stabilize. They are confined to lee and cross-loaded terrain features and can be avoided by sticking to sheltered or wind scoured areas.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood: Likely

Expected Size: 2 - 2