Reactive wind slabs have likely formed throughout the region in response to last weekends snowfall, warm temperatures and extreme westerly winds. At lower elevations, precipitation fell as rain and the surface now exists as a refrozen crust. The new wind slabs are likely most destructive in the north of the region where storm accumulations totaled around 30cm and ridgetop wind speeds peaked at 130 kmh. The reactivity of these new wind slabs will likely change with elevation and underlying snowpack structure. Due to limited observations, I have very little confidence in what that underlying structure may be, although faceting, crusts and surface hoar development have been reported from various parts of the region. The region is now seeing moderate outflow winds from the N-NE which may be redistributing some of the new snow onto opposite slopes. This makes thing tricky and you may find new wind slabs on unsuspecting slopes and terrain features. I were traveling in the mountains, I'd maintain an investigative approach and dig down to test for weak layers before committing to a slope. If you've been in the mountains, please share your observations on our
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