Avalanche Forecast
Regions: Cascades - South East.
The avalanche forecast has been updated Monday morning for the central east and southeast zone for a high danger in the near and above treeline. Travel in avalanche terrain is not recommended in these areas.
Detailed Forecast
Update Monday morning for the central east and southeast zone: The NWAC Blewett Pass and Mission Ridge stations, the Mission Ridge pro-patrol and Snotels in the southeast Cascades report 1-3 feet of new snow on Monday morning. Further moderate to heavy snow seems possible in these areas Monday morning. Along with strong E-NE winds this should make new wind slab likely or very likely on lee mainly west to south slopes. Storm slab is also likely or very likely on most slopes. The avalanche forecast for these areas will be updated to high in the near and above treeline and considerable in the below treeline in the central east and southeast zones.
In the northeast zone:: snow showers should give way to clearing skies and continued cold temperatures. Strong NE-E ridgetop winds should continue to transport the ample loose surface snow and build touchy wind slabs on more non-traditional or unusual SE-SW aspects, mainly above tree line and possibly near tree line.
Deep, low density snow will make sluffs or loose slides likely on steep wind sheltered slopes. Watch for travel on steep slopes above terrain traps, such as cliffs or creeks where the entertainment of loose snow may bury someone caught more deeply.Â
Fresh, touchy wind slabs near ridges and non traditional aspects, will be the primary avalanche problem on Monday. Wind affected snow should be widespread Monday, especially with strong shifting winds, watch for wind transported snow on a variety of aspects and cross loaded features.
Along all of the east slopes the 12/17 PWL persistent slab problem is gaining strength, becoming more deeply buried and less sensitive in snowpack tests. However, continue to avoid large open terrain in areas where an overall shallow snowpack exists, or where you find this layer in snow pits, especially if you experience direct observations such as whumpfing or shooting cracks.Â
Snowpack Discussion
Weather and Snowpack
Strong storms around the Solstice deposited generally half to 1 inch of water equivalent along the east slopes. Storm totals generally ranged from 6 to 12 inches.Â
A series of storms beginning last Monday have deposited 1-2 feet of snow over most east slope areas through Friday.Â
Clearing Friday night allowed areas of surface hoar to form in some zones below tree line, reported in the Washington Pass area Saturday.
A deep cold low pressure system has added another 5-15 inches of snow through New Year's Day. With the exception of crest level and exposed ridges, this recent snow has accumulated with a cooling trend and little wind effects.Â
Recent Observations
In the Delancey Ridge area in the Northeast zone Thursday, NCMG reported the new snow totaled 15-20 cm (6-8 inches) through the afternoon but was lacking a slab structure near and below treeline. In the same area Friday, small loose dry avalanches were the primary avalanche problem, but wind affected snow surfaces were visible above treeline. Besides loose dry avalanches in steep terrain, no evidence of natural avalanche activity was observed. In the Washington Pass zone, the 12/17 PWL has been found to be unreactive and has been removed from the set of avalanche problems. Â
Last week Mission Ridge ski patrol produced 1.5 to 3 ft hard slab avalanches during control work. These avalanches were releasing on basal facets about 15 cm from the ground. Â
On Saturday 12/24, a backcountry skier in the Lake Clara area near Mission Ridge reported a huge whumpfing noise, likely indicating a collapse of the basal facets. While no avalanche occurred, the terrain where the collapse occurred connecting to a large avalanche path that was NE facing near treeline.Â
Tom Curtis was out at Mt. Lillian Friday and found reactive wind slabs along ridges with shooting cracks and whumpfing on north aspects near 5900 feet. Â The wind slab was likely collapsing down to the 12/17 Persistent Weak Layer (buried surface hoar) about 25-35 cm down. Wind slabs were found on NW-E-SE aspects with some wind loading apparent well below treeline.
Touring in the Washington Pass area Saturday reported no results from hand shears in the near and below treeline bands and no avalanches while avoiding possible wind loaded terrain above treeline. Nice, low cohesion surface snow conditions were reported below treeline.Â
On New Year's Day, reports from multiple snow pits by Mission Ridge patrol testing the basal facet layer, now indicate a much stronger more settled snowpack from a week ago. The basal facets remain intact, but show signs of rounding and overall consolidation and bonding.
Avalanche Problems
Wind Slabs
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: Very Likely
Expected Size: 1 - 2
Storm Slabs
Release of a soft cohesive layer (a slab) of new snow that breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. 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.
You can reduce your risk from Storm Slabs by waiting a day or two after a storm before venturing into steep terrain. Storm slabs are most dangerous on slopes with terrain traps, such as timber, gullies, over cliffs, or terrain features that make it difficult for a rider to escape off the side.
Storm slabs usually stabilize within a few days, and release at or below the trigger point. They exist throughout the terrain, and can be avoided by waiting for the storm snow to stabilize.
Aspects: All aspects.
Elevations: All elevations.
Likelihood: Likely
Expected Size: 1 - 1
Persistent Slabs
Release of a cohesive layer of soft to hard 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 Slabs.
The best ways to manage the risk from Persistent Slabs is to make conservative terrain choices. They can be triggered by light loads and weeks after the last storm. The slabs often propagate in surprising and unpredictable ways. This makes this problem difficult to predict and manage and requires a wide safety buffer to handle the uncertainty.
This Persistent Slab was triggered remotely, failed on a layer of faceted snow in the middle of the snowpack, and crossed several terrain features.
Persistent slabs can be triggered by light loads and weeks after the last storm. You can trigger them remotely and they often propagate across and beyond terrain features that would otherwise confine wind and storm slabs. Give yourself a wide safety buffer to handle the uncertainty.
Aspects: All aspects.
Elevations: All elevations.
Likelihood: Unlikely
Expected Size: 1 - 1