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Avalanche Forecast

Archived

Apr 9th, 2014–Apr 10th, 2014

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.

A mix of winter like and spring conditions and concerns should be seen on Wednesday.

Detailed Forecast

Clouds should decrease near and west of the crest Wednesday morning. Partly or mostly sunny weather should be seen Wednesday afternoon with moderate temperatures and generally light west winds.

The dry weather and moderate temperatures should lower the avalanche danger a notch on Wednesday compared to the past few days.

But the sun is getting stronger and stronger now that we are well into April. The most extensive concern should be possible wet snow avalanches by Wednesday afternoon especially in new snow on solar slopes above treeline but in older wet snow on other slopes as well. Watch for wet surface snow deeper than a few inches, roller balls in surface snow and small natural wet loose releases that usually precede more major wet loose snow avalanches. Avoid terrain traps where a small but powerful wet loose avalanche could have unintended consequences. 

A less extensive second concern will be possible new wind slab from in the above treeline zone. This will be limited to lee slopes above treeline that get a few inches of snow. Watch for small areas of firmer wind transported snow.

New storm slab seems unlikely due to the cooling trend and limited amounts of new snow. But watch for small areas of short lived storm slab in more sheltered areas above treeline that get a few inches of snow.

Although it will not be listed as a primary concern continue to be wary of cornices. Cornice failures are often seen during the transition to spring weather. Cornices have grown large recently and often break back further from the edge than expected.

Snowpack Discussion

A front crossed the Northwest Friday. Another moist front crossed the Northwest Saturday afternoon and night. Water equivalents and snowfall for these systems at NWAC stations at higher elevations near and west of the crest were in the .7-2.4 inch and the 5-25 inch range respectively. Warmer temperatures were seen by Sunday and especially Monday. The recent snow and warmer temperatures caused avalanches. Some avalanches were triggered by cornice failures.

The Mt. Baker and Alpental ski patrols reported widespread wet loose avalanches Sunday afternoon. A couple of reports via TAY for Sunday and Monday also indicate wet loose avalanches on solar slopes in the central Cascades.

NWAC observer Jeff Hambelton was on Grouse Ridge near Mt. Baker Monday and reported a cornice fall that had triggered a D2 storm slab avalanche near treeline as well as wet loose debris. These avalanches likely occurred Sunday. Check out Jeff's latest video here.

Storm slab avalanche likely triggered Sunday by a cornice failure on Grouse Ridge. Photo taken Monday by NWAC observer Jeff Hambelton.

NWAC observer Dallas Glass is on Mt Baker Monday and today. He reported up to 15 cm of moist or wet surface snow and further natural wet loose avalanches on solar slopes on Monday. He also reported cornice triggered natural avalanches on Monday.

Less avalanche activity should be seen Tuesday as a front approaches the Northwest and clouds cut down on solar effects and temperatures begin to cool. The southwest to northeast oriented front should shift from the Olympics and north Cascades this afternoon to the south Cascades Tuesday evening. A few inches of snow is possible in the above treeline zone this afternoon through tonight.

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.

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.