Avalanche Forecast
Jan 26th, 2019–Jan 27th, 2019
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Regions
Stevens Pass.
The Bottom Line: Expect the warmest temperatures of the winter, so far. Warming, sun, and uncertainty of how the snow will respond at upper elevations is keeping the danger heightened. If you are heading to higher slopes, use caution on slopes 35 degrees and steeper.
Snow and Avalanche Discussion
With warming and sun, uncertainty about the snowpack is increasing. Most loose wet avalanches you will see are a few days old. Watch for wet avalanches if you see soft, wet snow on sunny slopes and at low elevations.
About 13” of snow, followed by rain on Tuesday night and Wednesday led to a widespread natural avalanche cycle throughout the Cascades. Many large paths in the area ran including Wellington, Highway Chutes, Lichtenberg Southeast side, Arrowhead Northeast Bowl, The Swath, and likely others. It rained up to around 5,500ft. Check out the Regional Synopsis tab for details on the storm and avalanche activity.
Problems
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of 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 Slab.