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

Mar 12th, 2019–Mar 13th, 2019

Alpine
Natural avalanches possible, human triggered probable.
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, human triggered possible.

Regions

.

Update: Decreased avalanche danger near treeline to reflect lower than anticipated snowfall amounts.

Expect dangerous conditions to develop at upper elevations, as a strong storm will increase the avalanche danger on Tuesday. The wind will transport a significant amount of snow-both new and old, and it may not bond well to the old surface. Choose a simple route plan for the day, one that allows for avoiding avalanche terrain at upper elevations. 

Discussion

Snow and Avalanche Discussion:

A major change is on the way. This storm headed our way will bring along sustained winds and a decent amount of new snow. More snow will fall in areas closer to the crest like the Salmon la Sac, Teanaway, and the Chiwaukum Range. East of Highway 97, much less new snow will fall. As such the danger may not reach Considerable there. The temperatures have been quite cold recently, and current snow surfaces are a mix of sun crusts on southerly aspects to weak, faceted snow on northerlies. Recently buried layers were also weak and faceted. The slightly warmer temperatures, and winds with this storm are ideal for slab formation. Now is as good a time as any to remember that most avalanches occur during, or directly after a snowfall event. 

On Sunday, observers triggered small lingering wind slabs on a north aspect of Wedge Mtn at 4,000ft. We haven't had any reports of collapses since last weekend, when observers reported signs of instability like collapses on Blewett Pass, Nahahum Canyon, and the northeast side of Wedge Mountain. Over this past weekend, the avalanche danger eased, and folks were able to get out and enjoy a couple of very nice days with good stability and great snow in the mountains. This storm may change that for a little while. 

Small wind slab triggered by a skier on a Northeast aspect of Wedge Mountain on 3/10. Notice the sparkly (faceted) snow surfaces. Photo: Matt Holland.

Snowpack Discussion

March 10, 2019

February started stormy and cold with very active avalanche conditions on persistent weak layers. The month finished with continued cold temperatures but drier weather allowed avalanche activity to taper off. Persistent weak layers that were buried early in the month (Feb 8th) are now unreactive, though you can still find the grains.

Aside from the series of storms in early to mid-February, most regions have measured relatively light snow accumulation in the past 3 weeks. Snow has stayed soft especially on shaded slopes and faceting and surface hoar have been plentiful. While there has been plenty of sunshine since mid-February, very cold temperatures have kept melt-freeze crust to a minimum on sunny slopes.

A natural loose wet avalanche (D1.5) on a southeast aspect of Lichtenberg Mtn at 5,400ft. 3/10/2019. Photo: Josh Hirshberg

Recent Avalanches

Our attention shifted to the upper snowpack. Recent avalanche problems have largely focussed on wind transported snow and weak snow surfaces on both dry, shaded slopes and sun-exposed aspects. In some locations, a weak layer of surface hoar and facets was buried on March 6th. We’ll keep an eye on this interface as we move into the future.

A skier-triggered storm slab avalanche (D1.5) on Shuksan Arm, north aspect, 5200ft. 03/09/19 Adam U Photo. 

Moving Forward

As we move further into March, there are two points to consider:

  • The strength of the March sun: As the sun creeps higher into the sky and the days grow longer, the sun can have a greater impact on the snow surface. When the sun comes out, expect things to change quickly. You may see avalanches conditions change with natural loose avalanches originating from sunny slopes, surface snow becoming thick and heavy, and slabs taking on a moist to wet snow character.

  • Weak surfaces: facets and surface hoar have blanketed snow surfaces in many zones. Any significant snowfall will bury well-developed and widespread persistent weak layers. Recently, most storms have not delivered enough precipitation to cause a problem.

Problems

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.