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Avalanche Forecast

Archived

Apr 6th, 2016–Apr 7th, 2016

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Olympics.

Heat related loose wet avalanches and cornice releases will be possible on Thursday. You will need to be able to evaluate avalanche conditions on specific terrain features and change your plans if snow conditions are more dangerous than expected.

Detailed Forecast

Sunny, warm weather is expected on Thursday.

Loose wet avalanches, mainly involving any recent storm snow from Monday and Monday night, will be possible on any steep slope, especially during the warmest part of the day Thursday afternoon. Pay attention to the integrity of surface crusts formed overnight. Backcountry travel early in the day is recommended since conditions can change rapidly due to daytime warming. Watch for wet snow deeper than your boot tops especially on steep solar slopes during the midday and afternoon hours.

The likelihood of cornice releases will continue on Thursday from intense solar radiation and warming temperatures. Cornice releases can be unpredictable during the spring so avoid areas below cornices and remember that cornices can break much further back than expected along ridges.

Any wind slab deposits caused from the snow received Monday, in combination with moderate westerly winds should have mostly stabilized by Thursday and wind slab won't be listed as an avalanche problem on Thursday. However, continue to watch for signs of wind slab mainly on north to east facing slopes above treeline where extra caution is warranted.  Firm wind transported snow and snowpack cracking can be good signs of wind slab layers.

Although not listed as an avalanche problem, large, powerful glide avalanches can release unexpectedly so avoid areas below steep unsupported slopes or rock faces.

Snowpack Discussion

Weather and Snowpack

A large upper ridge dominated the weather last week through early Sunday, resulting in warm and dry weather. A spring avalanche cycle occurred in most areas over this stretch, likely peaking midweek in the Olympic range. After a stormy March, the snowpack has undergone significant settlement and multiple melt-freeze cycles over the last week.

A front moved across the Olympics early Monday morning, resulting in a period of mostly light precipitation, cooling and moderate westerly crest level winds.

Another upper ridge is currently over the Northwest causing sunny weather and warm temperatures. 

The mid and lower snowpack in the Olympics should generally be a stable mix of crusts and layers of moist and rounded snow crystals.

Recent Observations

During the warm stretch last week, 1 large glide avalanche (R3-D3) naturally released on the 20th of June slide path (easterly aspect, near treeline) to the ground. According to NPS rangers, the avalanche likely released on Wednesday or Thursday.

NWAC pro-observer, Matt Schonwald toured extensively in the Hurricane Ridge area Saturday, 4/2 and found a well settled and seasonally deep snowpack with very few avalanche concerns.  

Only shallow amounts of recent snow were received Monday through early Tuesday at Hurricane Ridge. This lead to a slight increase in danger, mainly on specific terrain features such as any exposed lee slopes at higher elevations that received greater wind deposited snow. 

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

Cornices

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 drifts 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.