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Avalanche Forecast

Archived

Feb 29th, 2020–Mar 1st, 2020

Alpine
Natural avalanches possible, human triggered probable.
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 unlikely, human triggered possible.
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

North Columbia.

Limit your exposure and be disciplined with your terrain choices as you enjoy fresh snow. A buried surface hoar layer lurks and is easily triggered, producing large avalanches, especially where wind affected. Check out this Fx blog on Surface Hoar.  

Confidence

Moderate - Recent weather patterns have resulted in a high degree of snowpack variability within the region.

Weather Forecast

SATURDAY NIGHT: Cloudy with clear periods and isolated flurries, Trace accumulation. Winds light to moderate Northwest. Alpine low temperatures -12 with freezing levels to valley bottom.  

SUNDAY: A mix of sun and clouds with isolate flurries. Winds light to moderate West. Alpine High temperature -7 C with freezing levels near 800m

MONDAY: Cloudy with flurries, accumulation Trace to 10cm, with amounts diminishing to the south. Winds light to moderate Northwest gusting strong. Alpine high temperatures -5, lows to -11 and freezing levels rising to 1100m.

TUESDAY: Cloudy with localized Snow, accumulations Trace to 10cm, with amounts diminishing to the south. Winds Southwest Moderate to strong Southwest, gusting extreme. Alpine high temperatures -6 C and lows -9 with freezing levels rising to 1400m. 

Avalanche Summary

Early reports from Saturday suggest an increase in Natural and human triggered avalanche activity from recent snow and winds. Very Large (Size 3-3.5) natural and explosive controlled Avalanches were observed from extreme terrain in the higher mountains and along the highway corridor from North and South Aspects. There have also been numerous reports of large (Size 2) humanly triggered remote avalanches on the surface hoar issue at treeline and on North aspects .  

On Friday there were widespread reports of human triggered small (size 1-1.5) and large (size 2-2.5) avalanches, mostly failing on the Persistent Surface Hoar weak layer buried 30-45cm. These avalanches occurred on all aspects (South to North) and from 1000m to 2400m, with the largest occurring at ridge crests where snow was wind affected. There were a few large avalanches up to size 2.5 reported from steep Solar and North facing Alpine features.

Check out this MIN for an example of a recently reported avalanche on the Surface Hoar.  

Snowpack Summary

Recent snowfall amounts of 10-30 cm from Friday into Saturday's storm bring total snow overlying the widespread layer of Surface Hoar layer to 40-60 cm. Not only may there be weakness within this recent storm snow, but a significant load has been added to an already problematic Surface Hoar layer that was was reported to be between 10 and 20 mm in size. This Surface Hoar layer has been reported on all aspects at all elevation bands - but is most prominent near treeline and in sheltered alpine locations. On Solar aspects there is also a suncrust associated with the surface hoar, which is a nasty combination. Recent warm temperatures have built slab like properties in this snow, particularly at mid and low elevations, making the persistent layer more reactive.  

Across the region, this surface hoar layer is showing variability in its distribution and reactivity. This persistent weak layer has been most reactive to human traffic and natural trigger around treeline and alpine elevations where the overlying snow has slab properties and surface hoar is large. As this snow continues to gain slab properties activity on this layer is expected to increase and avalanches may grow in size.

The early-February melt-freeze crust down 50-100 cm is dormant but should be monitored. The remainder of the mid and lower snowpack is generally well-settled and strong.

Terrain and Travel

  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Avoid terrain traps such as gullies and cliffs where the consequence of any avalanche could be serious.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.

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.

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.