Glide Cracks
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1.5–2.5
The rapid warming produced wet loose avalanches, a few wet slabs, and then glide avalanches and cornice failures occurred, which produced subsequent avalanches. Large rollerballs and continued wet loose activity were reported in the West Central zone on Sunday. I saw new wet avalanche debris in the Highway 2 corridor on Thursday, which occurred in the last 48 hours. This was on a north-facing slope, and since we've gotten cloud cover we suspect more avalanche activity is happening on northerly aspects than was the case with clear skies.
Surface freezes on Wednesday night weren't as good as Tuesday night, since temperatures were slightly warmer and cloud cover trapped heat. A minimal freeze is expected for Friday. Without a surface crust, you could still trigger small wet loose avalanches. If you're sinking into soft wet snow stay away from steep slopes. Glide avalanches may fail up to a few days after a warming event, so continue to avoid terrain beneath large glide cracks, or travel through the area quickly. The same goes for large, saggy cornices.
Lower elevations are already so impacted by melting and have likely already fully run their course with wet snow avalanche problems.
(3/21/2024)
New wet avalanche activity on a north-facing slope at about 4500ft in the Highway 2 corridor. This happened in the previous 48 hours, after the large warming, but as the clouds created more of a greenhousing effect, with more moistenting on the northerly aspects.
Photo: Irene Henninger