Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Dec 11th, 2016–Dec 12th, 2016

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

Olympics.

Recent deep storm and wind slab deposits should be given ample time to settle and stabilize, especially due to the slow stabilization rates given the expected cold temperatures. Human triggered avalanches should remain likely on Monday. Choose low angled terrain and avoid slopes connected to avalanche paths with wind loaded start zones.

Detailed Forecast

Continued storm snow deposits overnight Sunday should give way to partial clearing Monday as high pressure affects the area. Winds should be light Sunday night and Monday with further cooling.   

While the ending showers with light winds and cold temperatures should lead to an overall improving avalanche danger Monday, there has been such significant storm snow, along with periods of moderate winds over the past three days, that another day or more of very cautious travel in backcountry terrain is urged.

Storm and wind slabs should begin to slowly settle and stabilize beginning Monday. However, careful snowpack evaluations, cautious routefinding and conservative decision-making will remain essential, as these dangerous avalanche conditions slowly improve.

Choose low angled terrain and avoid slopes connected to avalanche paths with wind loaded start zones. 

Loose dry will not be listed as an avalanche problem, but in steep terrain lacking a slab structure, continue to watch for small loose dry avalanches near terrain traps like cliff bands where even small avalanches can have big consequences. 

With deep unconsolidated snow in many wind protected areas, there remains an increased risk for tree well and snow immersion suffocation at this time. Ride or ski with a partner and keep them in sight at all times!

Even though the lower part of the below treeline band is filling in, watch for early season travel hazards such as barely covered rocks and open creeks.

Snowpack Discussion

Weather and Snowpack

An active and cool weather pattern has resulted in a snowy December thus far with the Hurricane Ridge NWAC station recording about 6 feet of snow, with over 3 feet in the past three days through Sunday afternoon! 

Cold and fair weather early last week likely allowed near surface faceting and/or surface hoar to become widespread. Beginning Wednesday night and through Thursday, considerable wind transport from easterly winds occurred near and above treeline. 

Beginning Thursday night and continuing on Friday, a switch to south-southwesterly winds occurred along with a moderate warming trend and light snowfall. 

Prior to this new snow, the snowpack in non-wind affected terrain was generally right side up with low density snow at the surface and no problematic layers in the lower snowpack.

Deep storm snow deposited over the past three days now overlies the old snow layers with storm snow of 2-3 feet or more common.   

Recent Observations

Moderate easterly winds midweek likely built new wind slabs on lee aspects near and below treeline in the Hurricane Ridge area with plenty of low density of snow available for transport. A switch to light S-SW winds late this week may have redistributed snow to more traditional NW-NE aspects Friday. 

This redistribution of recent and new snow continued on Saturday with additional new storm snow and moderate SSW winds. 

The Ranger at Hurricane Ridge indicated widespread natural slides had reached the road in many places by Sunday morning, likely releasing overnight during moderate to heavy snowfall and moderate winds.

We don't have any snowpack observations identifying persistent weak layers in the Hurricane Ridge area so we have a large amount of uncertainty whether new wind and storm slab avalanches will step down to deeper layers. 

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.