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Avalanche Forecast

Archived

Mar 23rd, 2020–Mar 24th, 2020

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.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

South Coast Inland.

New snow is creating heightened avalanche conditions, especially in southern parts of the region.

Confidence

Moderate - Uncertainty is due to limitations in the field data.

Weather Forecast

Unsettled conditions with light flurries for the next few days.

MONDAY NIGHT: Cloudy with variable flurries bringing anywhere from 0 to 15 cm of new snow, light west wind, freezing level drops to valley bottom, alpine temperatures drop to -8 C.

TUESDAY: Cloud with isolated flurries and variable accumulations of 0 to 10 cm, light north wind, freezing level around 1000 m, alpine temperatures reach -4 C.

WEDNESDAY: Mix of sun and cloud, light northwest wind, freezing level around 1000 m, alpine temperatures reach -4 C.

THURSDAY: Increasing cloud in the afternoon, moderate southwest wind, freezing level around 1000 m, alpine temperatures reach -4 C.

Avalanche Summary

No recent avalanches have been reported, but mountain travel and field observations have been very limited over the past few days. Last week there were many wet loose avalanches and some large glide slabs, but cooler weather and new snow has probably made new wind slabs the main concern this week.

Snowpack Summary

Current unsettled weather will continue to give localized accumulations of new snow on Tuesday, with the most probable accumulations around the southern part of the region (i.e. Cascades). Snowfall amounts as of Monday afternoon are 2-15 cm, and these amounts could double by Tuesday afternoon. The new snow is burying moist and crusty snow, as well as potentially some small surface hoar on shaded slopes at lower elevations. Overall, there is some uncertainty about how well the new snow will bond to these interfaces.

Northern parts of the region (e.g.. Duffey/Hurley/Gold Bridge) have had a deep instability lingering at the base of the snowpack for most of the season. While this layer has gained strength over the past month (the last reported avalanche was on Feb 17), it is still worth considering when assessing shallow, rocky slopes in this part of the region.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Closely monitor how the new snow is bonding to the old surface.

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.