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Avalanche Forecast

Archived

Dec 2nd, 2018–Dec 3rd, 2018

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Northwest Coastal.

We currently have very few observations in this region. Please post your observations to the Mountain Information Network. (MIN)

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Overnight SUNDAY: Clear / Alpine Low -12 / Light, northeast wind / Freezing level valley bottom.MONDAY: Sunny / Alpine high -10 / Light, northwest wind / Freezing level valley bottom.TUESDAY: Sunny / Alpine high -10 / Moderate, northwest wind / Freezing valley bottom.WEDNESDAY: Sunny / Alpine high -10 / Light, northwest wind / Freezing level valley bottom.

Avalanche Summary

No new avalanches were reported in this region on Saturday. However, we currently have very few observations from within this region. Please post your observations to the Mountain Information Network. (MIN)

Snowpack Summary

10-15 cm of recent storm snow is sitting on a thick, hard crust. Some reports indicate there may be an early season crust near the bottom of the snowpack.There is an average of 70-120 cm of snow in the alpine. This decreases dramatically with elevation where the primary hazards are rocks, stumps, and open creeks.We currently have very limited snowpack observations, so it is critical to supplement this information with your own observations.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.