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Avalanche Forecast

Archived

Dec 28th, 2017–Dec 29th, 2017

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

Regions

Olympics.

Human triggered avalanches will become more likely as denser storm snow continues to build over less dense older snow near and above treeline as snowfall intensities increase during the day Friday. Especially watch for building wind slab on a variety of aspects near and above treeline where either older less dense or newer denser snow has been transported onto lee slopes. As rainfall increases and moves to higher elevations tomorrow, watch for saturated snow and avoid consequential terrain features. Watch for changing conditions, travel conservatively and rein in your plans as conditions deteriorate throughout the day.

Detailed Forecast

A second storm (Friday) on the heels of the first (Thursday), will bring significantly more precipitation and further warming than the initial system. The storm track that will bring moderate SE winds shifting to SW during the day, along with further warming, increasing precipitation intensities, and snow lines rising above ridge crest level (at Hurricane) late in the day. Sharp cooling and drying should arrive during the evening hours.

Wind and storm slabs will be increasing in size and likelihood of human triggering as slabs of increasing thickness build over the lower density, weaker, older snow prior to Thursday and become increasingly touchy by later in the day. Especially watch for building wind slab on a variety of aspects as winds directions shift during the storm. Wind and storm slab issues will be confined to increasingly high elevations as the rain/snow line works it's way to higher elevations during the afternoon hours.

On Friday morning, loose wet avalanches are mostly likely encountered below treeline on steeper slopes due to warming and light to moderate rain. By afternoon, loose wet avalanches will be found further up the mountains in the near treeline band. At higher elevations which have received more snowfall, the loose wet slides will be larger and and increasingly consequential. In general, when snow is becoming saturated, avoid complex terrain as loose wet avalanches will be much more dangerous.

Watch for changing conditions, travel conservatively and rein in your plans if conditions deteriorate faster than expected. See the mountain weather tab for weather forecast details. 

Also despite all the new snow, early season hazards still exist at some lower elevation locales and especially around creek beds that are not filled in.

Snowpack Discussion

At Hurricane Ridge, the frontal system arriving Thursday evening brought a few inches of higher density snow at temperatures just below freezing, with light to occasionally moderate SW winds which transported some snow.

This new snow sits over the estimated 6 inches of lower density snow accumulation during the series of weak weather disturbances that traversed the area over the last week prior to Thursday. 

The previous major storm cycle ended 12/19-12/20.

Observations

On Wednesday, a shallow loose dry avalanche on a northwest aspect in the Tunnel Path above the road ran 100 feet and knocked a skier off his feet. A pit nearby showed right-side-up snow.

A second hand report of at least one human triggered loose dry avalanche (sluff) caught a skier(s) on Sunday 12/25. No injuries were reported. 

NWAC pro observer Matt Schonwald was at Hurricane Ridge on Saturday 12/24 and reported evidence of north to east winds but no wind slab or significant layers in the upper snowpack. The snowpack structure was generally right-side with good bonds to the Thanksgiving crust.

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.