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Archived

Avalanche Forecast

Jan 8th, 2017–Jan 9th, 2017
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
2: Moderate
The avalanche danger rating below treeline will be moderate
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
2: Moderate
The avalanche danger rating below treeline will be moderate

Regions: Mt Hood.

New wind slab is most likely on Monday on northwest to southeast slopes mainly in the near and above treeline. Avoid slopes above terrain traps in the below treeline where recently formed weak layers may have been buried by new snow.

Detailed Forecast

New snow by Monday morning at Mt Hood may be up to a foot or so. Temperatures will be cooler by Monday morning.

Southwest winds aloft should decrease on Monday. Moderate snow showers at Mt Hood should decrease on Monday with further cooling.

If you travel into the back country at Mt Hood Monday watch for new wind slab mainly on northwest to southeast slopes mainly in the near and above treeline. Previous wind slab may linger on other slope aspects also mainly in the near and above treeline. Watch for firmer wind transported snow.

New storm slab is possible Monday on sheltered slopes where there was more than several inches of rapidly accumulating snowfall.

New wind and storm slab layers should be more stable by the end of the day on Monday.

Remember that recently formed surface hoar and surface faceted snow has been seen lately in the Cascades in the below treeline. It will be a good plan to avoid slopes above terrain traps in the below treeline where these weak layers may have been buried by new snow.

Snowpack Discussion

Weather and Snowpack

A cold dry Arctic air mass was over the Northwest last week. The main weather event last week was a day or so of nuclear east winds on Wednesday that went on a powder wrecking rampage, scouring windward slopes, re-distributing it to lee slopes and building sastrugi in other areas.

Reports indicate the winds eliminated most of the faceted surface snow and surface hoar that formed in the near and above treeline during the cold weather. But these weak surface crystals are still reported in the Cascades below treeline.

A warm front is moving south to north over the Northwest on Sunday eroding and replacing the Arctic air mass and causing warmer temperatures. Southeast winds aloft on Sunday will shift to southwest by late Sunday and Monday.

Recent Observations

No reports were received on Wednesday and fierce winds that kept the ski areas from running most of their lifts also likely prevented anyone from venturing into the near or above treeline on Mt. Hood. 

NWAC pro-observer Laura Green was at the Mt Hood Meadows Ski Area on Thursday following some of the strongest winds experienced on Mt Hood for a very long time. She found a mix of wind sculpted conditions, ranging from deep hard slabs, likely 1-2 meters or more in depth as well as scoured slopes to crust layers, sastrugi, and a thin melt-freeze sun crust on many south aspects. These deep slabs are unlikely to be triggered by a solo traveler, however, more shallow wind slabs may be a different story. Settled and stable powder was found on wind sheltered terrain, where skiing conditions remained very nice.

Laura was out again on Friday in the Mitchell/Iron Creek area in the 4200-6000 foot range and found hard slab drifts from the high wind event of 1/4 even below treeline, and in reverse of what is usually present due to the east winds. She reported lots of variation in surfaces - wind hardened snow, sastrugi, bumpy ice, settled powder and tree debris. But no signs of instability were observed.

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: Likely

Expected Size: 1 - 1

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