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Avalanche Forecast

Archived

Mar 14th, 2020–Mar 15th, 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, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

Little Yoho.

Good travel conditions but cold temperatures on Sunday. Ensure you are prepared to stay warm in the event of any delay.

Ice climbers should be cautious with steep pillars which often respond poorly to cold temperatures.

Weather Forecast

Sunny skies and below normal temperatures will remain on Sunday with lows of -25 to -30'C and highs of -8 to -15'C. Wind will generally be light through all of the eastern slopes as the surface ridge stays firmly in place. Solar inputs may warm steep sunny slopes to near freezing in the afternoon.

Snowpack Summary

15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes. On steep solar aspects a thin sun crust is present. The deeper snowpack of Little Yoho is generally quite strong with few weaknesses.

Avalanche Summary

A couple small avalanches were observed Saturday. One natural size 2 slab released on a shallow steep SW aspect near Mt Hector, and a few small sluffs triggering thin thin wind slabs up to size 1.5 were observed near Bow Summit out of steep rocky terrain. Ski hills were able to ski cut a few thin wind slabs near ridgetops.

Confidence

Wind speed and direction is uncertain on Monday

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.