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Avalanche Forecast

Archived

Feb 22nd, 2013–Feb 23rd, 2013

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

Regions

Jasper.

If we get more snow than is forecast, the danger rating will increase. Assess wind-loading patterns carefully.

Weather Forecast

Friday evening may bring 10-20cm (10mm water equivalency), possibly more with local influences but precipitation amounts are uncertain. There is more confidence in severe SW alpine winds with brisk winds at treeline. Front expected to dissipate Saturday a.m.. Saturday to Monday will haveĀ  flurries and seasonal temperatures.

Snowpack Summary

Variable windslabs exist in the alpine and treeline locations. They are bonding well. Expect a short lived storm snow instablity to form with the current system. Weak facets dominate low elevations. Solid midpack bridges basal facets treeline and alpine.

Avalanche Summary

No Patrol Friday. Thursday's Marmot Basin Portal creek patrol revealed no new avalanches. No Patrol on Wednesday.

Confidence

Forecast snowfall amounts are uncertain on Saturday

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.

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.