Avalanche Forecast
Regions: Cascades - North East.
Increasing wind and showers may create unstable wind slabs at mid and upper elevations on Saturday. Expect increasing avalanche danger during the day. On Sunday, very dangerous conditions may develop as a strong and potentially very wet system impacts the area.
Discussion
Snow and Avalanche Discussion:
Winter is about to make a reappearance in the high country. A stormy weekend is on tap, with avalanche danger on the rise. For Saturday morning, you may find a good overnight refreeze at the lower elevations. Cooling temperatures and increasing winds with more snow at higher elevations may create wind slabs to be careful of. Dangerous conditions look to develop by Saturday night/Sunday in the mountains with potentially very heavy snowfall and rain. There is some uncertainty with the weather forecast, but if it all pans out, another round of heavy precipitation with warming temperatures and very strong winds are headed our way on Sunday. Large avalanches may become very likely, and may run to lower elevations.Â
Previously, our avalanche problems have been driven by warm temperatures and a melting snowpack. No recent slides have been observed by WSDOT crews working on the spring opening of Hwy 20. Continue to factor in all the mountain hazards that you may find in the spring. Large chunks of snow are calving off steep, rocky features, creek crossings are sagging, lakes are melting out, and glide cracks are opening up. Below treeline, the snowpack is melting away.
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
A bout of heavier precipitation with snow levels at around 6,000ft on Friday night may have created small wind slabs in alpine terrain. Another round of snow may arrive in the morning, with snow levels dropping to around 4,000ft. Gusty winds from the southwest or west will quickly transport the new snow into thicker drifts on lee sides of ridges and gullies. Be on the lookout for these especially at higher elevations, where significantly more recent snow may have accumulated. If you find recently formed drifts or instability such as long cracks from underfoot, avoid steep wind loaded features.
If the sun is out in the morning, be careful of steep east and south facing slopes with new snow, as small wet loose slides may become common.
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