Avalanche Forecast

Issued: Mar 10th, 2019 11:00AM

The alpine rating is below threshold, the treeline rating is below threshold, and the below treeline rating is below threshold.

Northwest Avalanche Center NWAC, Northwest Avalanche Center

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Small loose wet avalanches may occur naturally or be human triggered on steep sunny slopes; use caution around terrain traps like gullies and cliffs. Be suspicious of shallow snowpack areas with a dense slab over weak snow. If you experience whumphing collapses while traveling in lower angled terrain, avoid exposure to slopes steep enough to slide.

Summary

Discussion

Snow and Avalanche Discussion

Sunshine and slightly warmer temperatures are forecast again on Monday, increasing the likelihood of loose wet avalanches on steep sunny slopes. Increasing high clouds and alpine winds will decrease the loose wet potential later in the afternoon.

Pay attention if natural pinwheel or rollerball activity begins and move to different aspects or lower angled slopes. Avoid terrain exposed to gullies, rocks, or trees where the consequences of a small avalanche could be quite large.

In shallower snowpack areas, you are more likely to find and potentially trigger a persistent slab avalanche within the top 1 to 2 feet of the snowpack. A public observation of a human triggered slab avalanche came from a north aspect at 3200' just north of the Columbia River (Stacker Butte). We don't know what layer the slab avalanche failed on and the report is now several days old, but it's a clear reminder of weaknesses that remain in the upper snowpack. If you find signs of instability such as cracking and collapsing in shallower snowpack areas, dial back your terrain selection to lower-angled and well-supported slopes.

Forecast Schedule and No Rating

At this time, we do not have enough specific snowpack information to issue an avalanche hazard rating for the East Slopes South zone. However, even when No Rating is applied, applicable avalanche conditions and backcountry travel advice will be provided throughout the season. When weather systems produce very dangerous avalanche conditions in adjacent zones, NWAC will issue an avalanche warning for this zone as well.

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.

Valid until: Mar 11th, 2019 11:00AM