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Avalanche Forecast

Archived

Mar 4th, 2021–Mar 5th, 2021

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

South Coast.

With heavy precipitation and strong winds on Friday, natural avalanches are likely. Consider your ability to recognize and avoid terrain as travel in avalanche terrain is not recommended. 

Confidence

High - We are confident the likelihood of avalanche will increase with the arrival of the forecast weather.

Weather Forecast

A powerful storm is impacting the region

Thursday night: Overcast, 25-35 cm of snow possible over 1300 m with rain below, strong south wind.

Friday: Overcast, another 25-35 mm of precipitation with snow line dropping from 1500 m to 1000 m throughout the day, strong southwest wind with extreme gusts.

Saturday: Mostly cloudy, 10-20 cm of snow, moderate south winds, freezing level near 800 m. 

Sunday: Mostly cloudy, 10-20 cm of snow, strong southwest winds, freezing level near 800 m. 

Avalanche Summary

Natural and human-triggered avalanches are likely on Friday.

This MIN from Sky Pilot on Sunday describes cornice debris around 1600 m. 

There have been no reports of avalanche activity over the February 24th crust layer since last Thursday, when small to large (size 1-2) skier triggered avalanches were reported on all aspects.

Snowpack Summary

Areas at upper elevations could see as much as 40-60 cm of snow accumulate by the end day on Friday. Strong south winds will contribute to rapid slab formation, making natural avalanches likely. The combination of wind and snow has the potential to weaken cornices, which can act as triggers on slopes below.

Deeper in the snowpack, a widespread hard rain crust is buried that formed at the end of February. This crust can be found all the way to the tops of the North Shore mountains. Reports indicate that the snow above is bonding well to the crust. 

The snowpack below the rain crust is well settled and strong in most areas. 

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow, wind, or rain.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.
  • Watch for changing conditions today, storm slabs may become increasingly reactive.

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.

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.