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Avalanche Forecast

Archived

Apr 13th, 2018–Apr 14th, 2018

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

Regions

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Expect dangerous avalanche conditions at all elevation as significant precipitation continues to impact the area. Avoid all slopes greater than 35 degrees Saturday and limit your exposure to large overhead avalanche terrain.

Detailed Forecast

Spring weather and snowpacks can be tricky. General rules-of-thumb used during the winter often do not apply. With the amount of recent new snow and more on the way, this is a good time to be cautious. Avoid all slopes greater than 35 degrees and limit your exposure to large overhead avalanche terrain.

You will be able to trigger large wind slab avalanches Saturday on steep wind loaded slopes near and above treeline. Use visual clues such as blowing snow, new drifts, or fresh cornices to identify and avoid wind loaded features.

Fluctuating temperatures during the storm created an “up-side-down” snowpack with heavier strong snow over lighter weaker snow. This is a classic strong over weak slab avalanche scenario. You are likely to find this snowpack structure in all sheltered avalanche startzones above the rain line. Storm slabs will be easiest to trigger in the morning as strong overnight precipitation tapers off. Storm slabs may extend into the upper below treeline zone depending on air temperatures and precipitation type.

At lower elevations, expect wet surface snow conditions. New rollerballs, fresh fan shaped avalanche debris, and rain on snow are all key signs that loose wet avalanches are likely. Some loose wet avalanches this week have entrained large amounts of old wet snow and traveled father than normal.

Other spring time avalanche hazards exists. Glide cracks have formed on some slopes. Glide avalanches are difficult to predict and can release at any time. Limit your exposure to any slope with glide cracks. Creeks are beginning to open up at lower elevations. Choose your travel routes wisely if you are planning to over larger creeks

Snowpack Discussion

Over a foot (30cm) of new snow has fallen as of Friday afternoon with more on the way overnight. Moderate to strong winds during the storm transported snow forming wind slabs near and above treeline. This new snow is falling on a melt-freeze crust formed and buried on 4/11. The strength and thickness of this crust is largely dependent on elevation.

Mild weather earlier this week allowed the upper snowpack to gain strength. Observations show the snowpack is comprised of several melt-freeze crusts, refrozen snow, and strong rounded grains. This has created a strong spring-like snowpack. Avalanches should be limited to the snow above the most recent (4/11) crust layer.

Observations

North

On Friday Mt Baker Ski Patrol reported wind slabs up to 16” (40cm) deep near treeline.  Loose wet avalanches were observed below 4500 feet despite lower snow levels.

NWAC professional observer Lee Lazzara traveled in the Baker backcountry Thursday. Lee found 8 inches (20cm) of new snow well bonded to the old snow surface. While Lee did see wind slabs, no wind slab activity was reported. Warming air temperatures and thin clouds resulted in several small (D1) loose wet avalanches in the afternoon.

Stevens

NWAC forecaster Dallas Glass traveled in the Stevens Pass area Wednesday. Dallas found the upper 5 feet (1.5m) of the snowpack to be generally strong. He did not find any significant layers of concern below the wet surface snow.

 

 

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.

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.