Avalanche Forecast
Regions: Mt Hood.
Slab avalanches will become increasingly dangerous throughout the day as a colder, windier weather system impacts Mt. Hood. Steer away from any open slope greater than 35 degrees when you find or expect more than 6 inches of new or drifted snow.
Discussion
Snow and Avalanche Discussion
Mt. Hood is in the midst of a winter-like storm cycle. Several days of snowfall have brought minimal accumulations at 5500 ft, but accumulations are becoming significant as you gain elevation. Reports indicate that this snow is bonding well, but with temperatures dropping late Friday afternoon, subsequent snowfall will be available for transport and will not heal as quickly.
Weâre expecting more precipitation Friday night and Saturday. This next system should be colder and wetter than Fridayâs storm. Unfortunately, the models continue to struggle with each round of precipitation. We are confident that itâs going to be stormy, and that the additional precipitation will be enough to increase the avalanche danger throughout the day Saturday. Youâll need to pay attention to the conditions around you and determine if the weather youâre experiencing lies outside of the forecast. When you see observations that donât line-up with what you expected, dial back your travel to lower angled slopes and more sheltered terrain.
The wet weather pattern is expected to continue Saturday night and Sunday with more precipitation and a potentially strong warming trend. This will continue to increase the avalanche danger. As more snow piles up, and snow levels fluctuate, we could be looking at very dangerous avalanche conditions this weekend.
The winter-like weather comes on the heels of a very mild early spring. Cooling temperatures should help the old wet snow surface begin to freeze. This will take some time. As water continues to move through the snowpack, you could still see glide avalanches, loose wet avalanches, and opening creeks. In some areas, cliffs and steep rocky slopes continue to shed snow. Use caution if as you travel near any of these spring transition hazards. Snow cover below 4000' has been disappearing quickly and south facing terrain near ridgelines are melting out as well.
Snowpack Discussion
April 3rd, 2019
Spring snowmelt
The snowpack in much of the Cascades has changed dramatically in the past two weeks. The weather has shifted solidly to spring-like patterns. The spring warm-up started in mid-March with a prolonged period of relatively clear skies and warm temperatures. Moving into April, weâre seeing periods of unsettled spring weather bringing rain to many low and mid-elevation slopes and snow to upper elevations.
Very bare southeast aspects of Rock Mtn/Nason Ridge. April 2nd. Photo: Josh Hirshberg
Since the peak height of snow in mid to late February, mountain weather stations in the 4,000-5,000ft range show an average of 27% decrease in height of snow. Looking at weather stations in nearly every zone, the percentage decrease ranged from 22-29%. This year's spring snowmelt is much earlier than normal. Traveling in the mountains the loss of snow coverage is most noticeable on southerly, sun-exposed slopes and below 4,000ft. On northerly aspects and slopes above 5,500ft, the snowpack has seen less dramatic changes and has even maintained some dry layers.
NWAC climatological snow depth data from April 1st. You can view it on our website here.
Spring avalanche considerations
As you head into the mountains there are a few questions to ask yourself common to spring avalanche conditions:
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Is there any recent snow accumulation that could cause avalanches? If so, what kind of avalanches could you trigger? And where?
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What are the high and low temperatures of the past 24 hours as well as the forecasted temperatures during the time youâll be in the mountains? Could these create weak, wet snow surfaces?
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How is the cloud cover contributing to the melting or freezing of surface snow? Did clear skies allow for a sufficient overnight freeze? Will the sun be strong enough to weaken surface layers?
Glide avalanches and holes opening up in rocky terrain near Mount Herman. Photo: Andrew Kiefer
Other considerations
In addition to daily avalanche hazard, the early snowmelt is creating some other travel considerations. Some roads and lower elevation slopes may not have enough continuous snow coverage for travel on snow machines. Holes melted around rocks, trees, and creeks could create a fall hazard. When nighttime temperatures and cloud cover allow for surface freezes, bring appropriate equipment to mitigate slip and fall hazard on steep slopes.
We are approaching the end of our daily avalanche forecasting season. The mountain weather forecast will continue into the spring, and the weather station data is available year round. Keep checking the forecast for conditions updates on the end of season information.
Avalanche Problems
Wind Slabs
Cold temperatures, increasing precipitation, and strong winds Saturday will build large and dangerous wind slabs by the end of the day. You are most likely to trigger these near and above treeline where snow may be drifted deeply, but slabs will build down the mountain during the day, into the near treeline band. If you experience punchy snow or see evidence of recent or fresh snow transport, choose supported slopes less than 35 degrees. In sheltered areas, you can trigger a storm slab in areas receiving more than 6” of snow.
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: All elevations.
Likelihood: Likely
Expected Size: 1 - 1