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Archived

Avalanche Forecast

Nov 3rd, 2018–Nov 4th, 2018
Alpine
Below Threshold
The avalanche danger rating in the alpine will be below threshold
Treeline
Below Threshold
The avalanche danger rating at treeline will be below threshold
Below Treeline
Below Threshold
The avalanche danger rating below treeline will be below threshold
Alpine
Below Threshold
The avalanche danger rating in the alpine will be below threshold
Treeline
Below Threshold
The avalanche danger rating at treeline will be below threshold
Below Treeline
Below Threshold
The avalanche danger rating below treeline will be below threshold
Alpine
Below Threshold
The avalanche danger rating in the alpine will be below threshold
Treeline
Below Threshold
The avalanche danger rating at treeline will be below threshold
Below Treeline
Below Threshold
The avalanche danger rating below treeline will be below threshold

Regions: Jasper.

Snowpack Summary

Seasonal height of snow (HS) 77cm, with previous and new storm snow (HST) totaling about 40cm over a late Oct. (Oct 24) crust. Weak faceted crystals to ground. For more information on early season conditions visit avalanche.ca.

Avalanche Summary

Saturday, Nov. 3rd, technicians traveled at TL and into the lower alpine on Parkers Ridge. They found a weak, unsettled snowpack. Whumphing was noted at TL in open tress, on NE aspects. Pockets of windslab, Up to 20cm deep was observed in the alpine with moderate loading expected to continue into the week.

Confidence

Avalanche Problems

Wind Slabs

Loaded gully features and a stiffening snowpack over waterfall and glacier ice are common traps for early season Ice Climbers. Consider an alternative route if overhead loading is possible.
Be careful with wind loaded pockets while approaching and climbing ice routes.Ski penetrations may be to ground in some areas due to weak and unconsolidated snowpack.

Aspects: North East, East, South East, South.

Elevations: Alpine, Treeline.

Likelihood: Unlikely - Possible

Expected Size: 1 - 2

Persistent Slabs

Noted sensitivity to skier travel at TL elevations.
Whumpfing is direct evidence of a buried instability.Ski penetrations may be to ground in some areas due to weak and unconsolidated snowpack.

Aspects: North, North East, East, North West.

Elevations: Treeline.

Likelihood: Possible - Likely

Expected Size: 1 - 2