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Archived

Avalanche Forecast

Dec 13th, 2018–Dec 14th, 2018
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
1: Low
The avalanche danger rating at treeline will be low
Below Treeline
1: Low
The avalanche danger rating below treeline will be low
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
1: Low
The avalanche danger rating at treeline will be low
Below Treeline
1: Low
The avalanche danger rating below treeline will be low

Regions: Olympics.

Avoid cornices along ridges built by strong winds and snowfall.  Watch for wind drifted snow in steeper terrain. Be cautious due to variation in snow cover and exposed rocks and vegetation. 

Discussion

Discussion 

Low snow conditions continue to limit the overall avalanche hazard in the Olympics. A little over a foot of new snow has accumulated in the Hurricane Ridge area since Tuesday, with periods of very strong southerly winds. There is a very wide degree of variation in snow cover based on elevation and especially aspect. On windward southerly facing terrain, much of the area is void of snow cover. While on shaded and wind loaded north to east facing terrain the snow-depths averaged about 4 feet as of Thursday afternoon. Avalanches are possible in wind loaded terrain, especially near and above treeline.  

Forecast schedule

For the 2018-19 winter season, avalanche hazard ratings will be issued for the Olympics Friday through Sunday and during holidays.

On days that the Hurricane Ridge road is closed, No Rating will be applied. We will continue to provide general snowpack and weather summaries for the Hurricane Ridge area even when No Rating is issued. 

Snowpack Discussion

Regional Synopsis 20181213

Winter is here.

A productive winter storm pattern has elevated the avalanche danger and provided an interesting start to the season.  

A quick breakdown:

  • Tuesday and Wednesday saw a significant localized avalanche cycles.

  • We have a lot of new snow...2’ to 5’ above 4500ft.

  • We’ve gotten a lot of wind.

  • We have weak layers near the ground.

Dangerous avalanche conditions will persist over the next couple of days. That said, it is early season and the flavor of avalanche you may run into is likely a function of elevation, timing, and dumb luck.

Here are some basic emerging patterns:

  • Snowfall totals so far this week (Monday morning to Thursday evening) illustrate more recent snowfall in the north than the south:

    • Mt. Baker: 55”

    • Washington Pass: 29”

    • Stevens Pass: 37”

    • Snoqualmie Pass: 28”

    • Paradise: 38”

    • Mt. Hood Meadows: 13”

  • Upper versus Lower Elevations: The change in the snowpack is still 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.

  • East versus West: Loading along the East slope has been more incremental, and a  variety of buried facet and surface hoar layers may be found. This is most pronounced near WA Pass. Although significant snowfalls and precip totals have resulted in thicker, more homogeneous snowpack in the western zones, lingering weak layers near the ground will persist through the week.

The uncertainty of how reactive our buried weak layers are will carry into the weekend. Be cautious and get home safe.

 

Avalanche Problems

Storm Slabs

Highly variable snow-cover exists in this zone. Don't be surprised by bare ground on many windward slopes with 4-5 foot wind drifts on leeward slopes below ridges. These are the areas where you can encounter and trigger a storm slab. Watch for wind stiffened surface snow and smoothly rounded wind-drifts. 

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: North, North East, East.

Elevations: Alpine, Treeline.

Likelihood: Possible

Expected Size: 1 - 1

Cornices

Cornices are growing large enough to trigger along ridges. Avoid travel on these cornices that are now extending over the ridges by several feet in places. Cornices are likely to be found along north to east facing ridges in higher terrain in this zone.

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind lips of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.

 

Cornices can never be trusted and avoiding them is necessary for safe backcountry travel. Stay well back from ridgeline areas with cornices. They often overhang the ridge edge can be triggered remotely. Avoid areas underneath cornices. Even small Cornice Fall can trigger a larger avalanche and large Cornice Fall can easily crush a human. Periods of significant temperature warm-up are times to be particularly aware.

 

A corniced ridgeline. A large cornice has formed at the top of the ridge. A smaller cornice has formed to the left of the trees from crossloading.

Cornices are easy to identify and are confined to lee and cross-loaded ridges, sub-ridges, and sharp convexities. They are easiest to trigger during periods of rapid growth (new snow and wind), rapid warming, and during rain-on-snow events. Cornices often catch people by surprise when they break farther back onto flatter areas than expected.

Aspects: North, North East, East.

Elevations: Alpine, Treeline.

Likelihood: Likely

Expected Size: 1 - 1