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Avalanche Forecast

Archived

Apr 13th, 2019–Apr 14th, 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.

Incoming snow should improve ski quality in the short term. Expect wind slab development late today and into Sunday.

Weather Forecast

Snow changing to rain showers near noon with snowfall amounts near 5cm. Freezing levels are expected to rise to 1400m to 1800m this afternoon depending which forecast you trust. Alpine temps should be in the -3C range with gusty SW winds up to 50km/h.  Gusty SW-W winds with continued light snow are forecast through to the end of the day tomorrow.

Snowpack Summary

Last week's storm snow has formed pockets of windslab lee slope alpine and treeline locations. Expect a melt freeze crust on true solar aspects at treeline and alpine locations. Protected high north aspects are the best bet for late season powder. Below treeline a melt freeze crust covers isothermal snow on all aspects.

Avalanche Summary

No new avalanches observed or reported yesterday.

Confidence

Problems

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.