Avalanche Forecast

Archived

Mar 18th, 2013–Mar 19th, 2013

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural and human triggered avalanches likely.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Regions

South Columbia.

Confidence

Fair - Forecast snowfall amounts are uncertain on Wednesday

Weather Forecast

Tuesday: Mix of sun and cloud / Light to moderate southwest winds / Freezing level at 1200mWednesday: Moderate to heavy snowfall / Strong to extreme southwest winds / Freezing level at 1500mThursday: Light snowfall / Light to moderate west winds / Freezing level at 900m

Avalanche Summary

A widespread slab avalanche avalanche cycle to size 2 took place on Sunday. The activity occurred in response to new snow and variable winds at all elevations. One notable occurrence was a size 3 slab avalanche which took place in the southeast corner of the region. The avalanche occurred on an east-northeast aspect at 2500m and was likely triggered by rapid loading from strong northwest winds. Observations were limited, but its size may suggest that a persistent weakness was the failure plane.

Snowpack Summary

Light to locally heavy amounts of new snow fell over the weekend and have have been distributed by northerly winds into deeper windslabs in lee terrain. These recent accumulations overlie a thick rain crust which is reported to extend up to 2000m. About 1m below the surface is a layer surface hoar or a sun crust buried on March 10th. Avalanche activity has become less likely at this interface; however, isolated natural activity and remote triggering is still occurring in some areas. At lower elevations where last week's heavy rain saturated the snowpack, subsequent cooling has formed crusts and has dramatically strengthened the snow.Weaknesses deeper in the snowpack have become unlikely to trigger.Widespread cornice development has also taken place, and cornices are reported to be very large and weak.

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.

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.