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Avalanche Forecast

Archived

Feb 13th, 2018–Feb 14th, 2018

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

Stevens Pass.

Avalanche conditions will change Wednesday due to a quick moving frontal system bringing fresh snowfall to the Cascades. Heightened avalanche conditions will exist on any slope greater than 35 degrees where significant new snowfall bonds poorly to the underlying surface including older weaker snow or a smooth crust.

Detailed Forecast

Avalanche conditions will change on Wednesday as a quick moving frontal system brings fresh snowfall to the Cascades Tuesday night and Wednesday along with much cooler temperatures.

On average, 6 to 12 inches of new snow may bond poorly to a medley of snow surfaces including weak surface snow in the form of persistent grain types, wind sculpted snow surfaces or various surface crusts. Heightened avalanche conditions will exist on any slope greater than 35 degrees where significant new snowfall bonds poorly to the underlying surface. 

Shallow storm slabs will be more sensitive to human triggering in specific areas if they develop over weaker snow (near surface facets) found in wind sheltered, non solar aspects. Also watch for developing storm slab instabilities in areas that experience extended periods of intense snowfall. 

While winds are not forecast to be especially strong with this system, westerly winds should build fresh wind slabs on lee slopes near and above treeline. Avoid steep slopes with wind deposited snow such as below cornices, on wind drifts, and near uneven snow surfaces. Wind slabs will be more likely to trigger in areas where wind deposited snow bonds poorly to an underlying crust or weak surface snow. 

Loose dry avalanches will not be listed as a problem but will be possible on very steep slopes. Be aware of the consequences of a loose dry avalanche near terrain traps such as cliffs, gullies, or open creeks. In areas where shallow loose new snow bonds poorly to the underlying crust, avoid steep icy slopes where it will be difficult to stop a fall. 

Continue to avoid other non-avalanche-related hazards such as glide cracks, creeks, and openings within the snowpack formed during warm wet weather in early February. Falling into these holes poses a danger to backcountry travelers. 

Snowpack Discussion

Heading into Tuesday night's storm, a strong and stable snowpack exists around the region. Up to 6 inches of older weak snow sits on the supportable 2/8 crust in most wind and sun sheltered locations along the west slopes of the Cascades. On slopes that have received direct sun over the past few days, spring-like conditions have developed. Above treeline and to a lesser extent near treeline, a medley of wind sculpted snow surfaces or surface crusts exist.

Warm wet weather from the beginning of February created a well consolidated snowpack. While we are tracking some deeper buried crust layers, there are no significant layers of concern.

There have not been any reports of avalanches in several days.

Observations from the West Slopes of the Cascades

NWAC field staff over the last several days have reported a strong snowpack and no recent avalanche activity throughout the west slopes of the Cascades. Older debris from the 2/4 avalanche cycle is still visible in many areas.

In non-wind or sun affected terrain, several inches of weak surface snow sits upon the 2/8 crust mainly in the form of near surface facets although some observations of surface hoar were also noted. NWAC staff in the Mt. Baker and the Paradise backcountry near and above treeline on Tuesday reported landscapes reshaped by recent winds and sun. Highly variable snow surfaces consisted of melt-freeze crusts, sastrugi, old wind deposits and scoured surfaces exposing slick crusts to name a few.  

Over the weekend, numerous glide cracks and openings in the snowpack were present and created a non-avalanche travel hazard.

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). 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.