The Bottom Line: We haven't had much weather in the last several weeks (in fact, this was our least-snowy January on record). Luckily, we got 4-5" of new snow last week to freshen up the slopes. Avalanche conditions haven't changed. We still have patches of buried surface hoar to worry about, and the usual surface wind slabs on high, wind loaded slopes.
The NW winds are still actively creating new wind slabs, and a few new natural and human-triggered slides were reported this week. Keep your guard up this weekend. Many areas will be stable and it will be tempting to venture onto larger slopes. But you can still trigger a deadly avalanche if you venture over areas of buried surface hoar. Be cautious out there, and perform tests on the upper snowpack to look for easy shears. Expect high variability from slope to slope, and avoid convexities. Practice good risk management: limit your exposure to dangerous terrain, and plan for the worst.
Problem #1: Wind Slab
Location: Wind-loaded and cross-loaded slopes (E-SE-S-SW aspects) steeper than 30 degrees.
Strong NW winds over the last two weeks caused loading of wind slabs onto lee aspects. Because the winds were so strong, loading patterns are likely to be unusual, so look out for wind slabs that get thicker/sketchier mid-slope, further down below ridgelines than usual. Convexities tend to collect wind slabs and act as trigger points. Some of these slabs could be 30-60cm thick. They will be sliding on old weak/facetted snow and patches of surface hoar.
Problem #2: Persistent Slab
Location: ALL elevations, clearings in the trees, and specific slopes above treeline (mainly slopes sheltered from NW winds) where surface hoar formed in Late-January and wasn't blown away by NW winds.
There are patches of buried surface hoar lingering underneath two layers of recent snow (roughly 15-60cm deep). We observed areas of natural wind slab avalanches running in low-angle terrain as mellow as 25-degrees, indicating how slick this weak layer is. It's distribution is sporadic and depends on how sheltered a slope was to NW winds. This dangerous weak layer will persist for several weeks or until it can be crushed and flushed out by lots of heavy snowfall. Keep this layer in mind over the next few weeks, and be sure to dig around in wind sheltered areas to look for it. Surface hoar is sneaky because it's hard to map out, but easy to trigger. Use extra caution in openings around treeline, and avoid wind-sheltered rollovers in the alpine.
Photo: human-triggered persistent slab on low-angle terrain in the Chilkat Pass zone. 2019-1-27
Over the last two-three weeks, we've had reports of isolated surface wind slab avalanches (D1-D2), both natural and human-triggered, in top-loaded and cross-loaded terrain between 2500-5000ft. Some wind slabs were sliding on low-angle slopes as low as 25 degrees, and appeared to be sliding on a buried surface hoar layer 10-30cm deep. Distribution of these avalanches was limited to wind loaded areas that had been protected from strong N/NW winds.
We've had 6 weeks of cold and mostly dry weather. The drought continues, but no worries because ski conditions have been great. Our last snowfall was 4-5" that fell about a week ago and freshened up the slopes. More clear and chilly weather is in store for this weekend, with continuing moderate NW winds. A strong but fast-moving front will bring snow Sunday night, probably 3-8".
( *star means meteorological estimate )
If you get out riding, please send in an observation!
Do a rescue practice with your partners. Always carry a beacon, shovel, and probe, and KNOW HOW TO USE THEM.
Practice good risk management, which means only expose one person at a time to slopes 30 degrees and steeper, make group communication and unanimous decision making a priority, and choose your terrain wisely: eliminating unnecessary exposure and planning out your safe zones and escape routes.
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