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Avalanche Forecast

Archived

Apr 15th, 2024–Apr 16th, 2024

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

Regions

Haines Pass.

Conservative terrain travel is recommended, as riders could trigger buried weak layers.

Confidence

Moderate

Avalanche Summary

Many natural and rider-triggered avalanches released last Thursday on the weak layers described in the Snowpack Summary (see photos below). These weak layers may take some time to strengthen, meaning they will likely remain active to human traffic for the foreseeable future.

Please consider sharing your observations to the Mountain Information Network.

Snowpack Summary

Recent storm snow has been redistributed by southerly winds and has likely formed wind slabs adjacent to ridges. The snow surface on sun-exposed slopes will likely become moist during the day and freeze into a hard melt-freeze crust overnight.

Weak layers of surface hoar crystals and/or faceted grains may be found around 30 to 70 cm deep. The weak layer may be associated with a hard melt-freeze crust above or below. These layers produced recent avalanche activity and are unstable in snowpack tests.

Cornices are large and looming at this time of year.

Weather Summary

Monday Night

Clear skies. 10 km/h west ridgetop wind. Treeline temperature -8 °C.

Tuesday

Clear skies. 10 km/h southwest ridgetop wind. Treeline temperature -4 °C.

Wednesday

Mostly clear skies. 20 to 30 km/h south ridgetop wind. Treeline temperature -2 °C. Freezing level rising to 1000 m.

Thursday

Clear skies. 30 km/h south ridgetop wind. Treeline temperature 0 °C. Freezing level rising to 1300 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Potential for wide propagation exists, fresh slabs may rest on surface hoar, facets and/or crust.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.
  • The more the snow feels like a slurpy, the more likely loose wet avalanches will become.

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.