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RegisterApr 6th, 2019–Apr 7th, 2019
Olympics.
A strong spring storm has created dangerous avalanche conditions in the Hurricane Ridge area. You can trigger a wind slab avalanche on steep slopes with drifted snow or a wet loose avalanche on any steep sunny aspect with wet snow. Think about the consequences of a small avalanche; on many sunny aspects and below 4500', the new snow will (barely) cover an array of ground hazards.
Hurricane Ridge had picked up at least 8" of snow by 5 pm Saturday. Earlier in the day, NPS Rangers had reported significant wind transport with a snow level between 3000-3500'. The new snow will temporarily refresh the rapidly retreating snowpack in the Hurricane Ridge area. Cool temperatures will preserve new storm instabilities while the opportunity for afternoon sunshine will increase the chances for wet snow avalanches.
Prior to this storm, large terrain obstacles were readily exposed with plenty of bare ground showing. North and northeast slopes had many glide cracks, but these can be present on any aspect. Reports from around the region have indicated that creeks are gushing and opening up with snow bridges collapsing. Cornices are sagging. Use caution if you travel near these features. Expect low snow cover everywhere below 4500 ft. Keep in mind that smaller features may be covered up by the recent snow.
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, we’re 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:
Is there any recent snow accumulation that could cause avalanches? If so, what kind of avalanches could you trigger? And where?
What are the high and low temperatures of the past 24 hours as well as the forecasted temperatures during the time you’ll be in the mountains? Could these create weak, wet snow surfaces?
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.