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Avalanche Forecast

Archived

Apr 14th, 2019–Apr 15th, 2019

Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.

Regions

Glacier.

Storm snow should soften skiing old frozen snow surfaces. Watch for storm slabs on the immediate lee of alpine ridges and exposed treeline locations.

Weather Forecast

Periods of snow ending late this morning with overcast skies and flurries this afternoon. Freezing level should rise to 1400m this afternoon with an alpine high of -6C along with moderate westerly winds. A mix of sun and cloud for Monday and Tuesday with freezing levels rising to 2000m by Tuesday afternoon.

Snowpack Summary

10cm+ of storm snow overnight with mod to strong SW-S winds will be forming soft storm slabs on alpine and treeline lee slopes. Melt freeze crusts on steeper solar aspects and all aspects below treeline. The BTL crust may be weakened from being insulated by storm snow. Below treeline a melt freeze crust covers isothermal snow on all aspects.

Avalanche Summary

No new avalanche activity observed or reported in the last 24hrs.

Confidence

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.