Avalanche Forecast
Regions: Olympics.
Wind slabs may be easier to trigger than you expect with an uptick in avalanche danger on Friday. Wind transport could form shallow slabs on weaker snow, allowing shallow slab avalanches to trigger easily. Avoid steep or unsupported slopes where you find wind-drifted snow.
Discussion
The Olympics are likely to pick up several inches of low-density snow overnight with snow flurries and mostly cloudy weather for Friday. The new snow and dry older snow on northerly aspects are being transported by moderate to strong SSW and W winds.Â
NWAC and Park Rangers on 12/26 reported that most slopes ran during an intense storm that dropped 33â of snowfall from December 18-21st. New snow filled in the paths and bonded well to the bed surfaces. Avalanches were up to size 2.5 (large to very large). With cool and mostly dry weather following the storm (only a skiff of new snow registered on Wednesday), snow near the surface has been losing strength.Â
Below 4000â a thin snowpack still exists, so continue to travel cautiously at lower elevations.
Forecast Schedule
For the 2019-20 winter season, avalanche danger ratings will be issued for the Olympics every Friday through Sunday and during mid-week holidays. During the week, No Rating will be issued but forecasts will include expected conditions and relevant travel advice. If you are out in the Olympics, share your backcountry observations with us and the greater community.
Snowpack Discussion
December 26, 2019 (The regional synopsis is updated every Thursday @ 6 pm)
No matter where you are in the northwest, the snowpack looks a world different than it did a week ago. A major storm, widespread avalanches, developing weak layers, and an initially thin snowpack made for a hectic week. Letâs take a look at a few large scale trends for our holiday season.Â
A very large natural avalanche (D3) on the Shuksan Arm near Mt Baker that occurred during the storm cycle. Photo: Adam U.Â
Wet and Wild
âSome of the highest precipitation rates Iâve ever seen.â âAbsolutely puking!â âRivers running in the streets.â âSnowing snow hard I canât see my hand in front of my face.â These were all statements we heard describing the wet and wild storm that impacted the Northwest from about Thursday (12/19) through Sunday night (12/22). Water totals were staggering in many locations (Table 1). For Hurricane Ridge, Mt Baker, Washington Pass, and high elevation terrain this deluge translated into significant snowfall. However, warm air in the central and southern parts of the region brought rain well into the near treeline bands. Whether your favorite spot saw rain or snow, four things are clear. 1. This was a huge loading event. 2. A widespread natural and triggered avalanche cycle (up to D3) occurred. 3. Avalanche danger spiked during and just after the storm before trending down through the week. 4. The snowpack changed dramatically.Â
Location
Precipitation 12/19-22
Hurricane Ridge
4.97â
Mt Baker Ski Area
7.35â
Washington Pass
3.53â
Stevens Pass
6.28â
Leavenworth
2.94â
Snoqualmie Pass
7.89â
Crystal Mt Ski Area
7.45â
Paradise, Mt Rainier
6.57â
Mt Hood Meadows
2.18â
Table 1: Precipitation totals for select weather station locations December 19-22. Â Â
The Emergence of Persistent Slab Avalanche Problems
Coming out of this huge loading event, there was hope that many of the early season weak layers had been destroyed. Unfortunately, this was not the case in some locations. Old weak snow layers reared their heads in areas east of the Cascade Crest and near Crystal Mountain. While the exact extent and character of these layers can differ slightly, most locations are finding a layer of weak sugary facets associated with a crust about a foot above the ground. Persistent slabs are tricky to assess. Do not solely rely on snowpits and snowpack tests to help you choose terrain. How will these layers change going forward? Only time and observations will tell.Â
You may find weak sugary facets near a crust about 12 inches above the ground similar to what you see here. Photo: Jesse Charles
Low Tide Snowpacks During the Holidays
The storm this past week definitely helped the meager early-season snowpacks in all locations. Areas like Hurricane Ridge, Mt Baker, and Washington Pass experienced a jump of 20 or more inches in their snow depths over the past week. However, even with these increases, an early season snowpack still describes most locations. Expect numerous obstacles as you travel including open creeks, rocks, and trees. With this thin snowpack, limited access, and difficult travel we still have limited observations in some regions.Â
Open, deeply incised creeks in the Alpental Valley. Photo: Dallas Glass
Lack of information leads to a higher than normal degree of uncertainty. If you travel to higher elevations or more remote trailheads, recognize you could experience different conditions than the forecast suggested. You can help us fill in the gaps by submitting your observation here.Â
Happy Holidays!Â
-Dallas Glass
Avalanche Problems
Wind Slabs
While the incoming system doesn’t have a lot of moisture to work with, it will bring enough wind to transport the low-density snow. Small wind slabs may be easy to trigger if they build on top of weaknesses near the surface of the snowpack. These wind slabs should be of greatest concern on steep or unsupported slopes near and above treeline where 4” of snow has accumulated. Watch for evidence of wind-textured snow surfaces, recently formed cornices, or active snow transport. On northerly aspects, weaker snow surfaces developed during the recent week of cool, calm weather. On southerly aspects, facets developed under a surface crust which will be very touchy if loaded by a wind drift. Consider your terrain selection with care as small, surprising avalanches can push you into terrain obstacles or traps.
In steep terrain without wind effect, you might trigger a Loose Dry avalanche.
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.
Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas..
Wind Slab avalanche. Winds blew from left to right. The area above the ridge has been scoured, and the snow drifted into a wind slab on the slope below.
Wind slabs can take up to a week to stabilize. They are confined to lee and cross-loaded terrain features and can be avoided by sticking to sheltered or wind scoured areas.
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1