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Avalanche Forecast

Archived

Feb 4th, 2018–Feb 5th, 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 possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

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Slowly lowering freezing levels and light amounts of new snowfall will decrease the overall avalanche danger Monday. The wet upper snowpack will begin refreezing Monday, but loose wet avalanches are possible on steep slopes with wet surface snow, especially in the morning. Avoid slopes where avalanches may carry you into a terrain trap. Fresh and shallow wind slabs are possible on lee slopes above treeline mainly in the central-east Cascades nearest to the crest. 

Detailed Forecast

Slowly lowering freezing levels and light amounts of new snowfall will decrease the overall avalanche danger Monday in the central-east and southeast Cascades.

The wet upper snowpack will begin refreezing Monday, but loose wet avalanches are possible on steep slopes with wet surface snow, especially in the morning. Avoid slopes where avalanches may carry you into dangerous terrain such as over a cliff, into a creek, or down a gully. 

Fresh and shallow wind slabs are possible on lee slopes above treeline mainly in the central-east Cascades nearest to the crest. 

Snowpack Discussion

Moderate to strong westerly winds at crest level built new wind slabs in the near and above treeline terrain in the northeast Cascades over the weekend. Precipitation was heaviest near the Cascade crest with precipitation rates quickly decreasing further to the east. Little snow was available to transport in areas further south of Holden. Over the weekend and peaking on Sunday, the snow level rose to 5500-6000 feet in the northeast Cascades, increasing to 6000-7000 feet further south and east. Wet snow conditions were noted near and below treeline along the Hwy 20 corridor with a wet loose cycle noted below 5500-6000 feet Sunday. 

A natural avalanche cycle has been reported in many areas from Monday’s (1/29) warm and wet weather. Rain occurred along the east slopes as far north as Holden, WA.

Scattered observations from the last week of January found buried surface hoar on top of the 1/16 crust. This persistent weak layer was found or thought to be the cause of several avalanches. Extra caution should be taken when traveling in areas further east of the crest where this layer may survive. Snow profiles and snowpack tests are the only means to identify and locate this layer.

Observations

North

On Sunday, snow professionals at the Barron Yurt near Hart's Pass reported stormy conditions with denser snowfall increasing the likelihood for storm slabs during the day due to rising temperatures in and around the 6000' level. Moderate winds were continuing to transport snow onto lee slopes near and above treeline. No deeper instabilities were noted in snowpack tests. Observations were limited in this terrain due to poor visibility. On Sunday in terrain further to the east, a wet loose cycle was noted below 6000'. 

On Saturday, snow professionals at the Barron Yurt near Hart's Pass reported about 6" of new snowfall over the preceding 24 hours. Touchy wind slabs were present near and especially above treeline with moderate to strong W-SW winds transporting new and recent snow onto lee slopes. Storm slabs were generally unlikely to trigger. The 1/16 crust was 4 to 5 feet down. Similar conditions were reported Friday in this area. 

Central

An avalanche professional traveling in Icicle Creek Thursday found 6-8” of settled snow well bonded to the 1/29 crust. Observations demonstrated a strong upper snowpack. No buried surface hoar was found in this location.

On Tuesday, Mission Ridge Pro Patrol identified several layers of concern in this regionally shallower snowpack. These layers should be watched during future loading events. Similar basal weak layers were found in the nearby shallow snowpack of Blewett Pass.

South

No recent observations

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.