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Avalanche Forecast

Apr 7th, 2016–Apr 8th, 2016
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
2: Moderate
The avalanche danger rating below treeline will be moderate
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
1: Low
The avalanche danger rating below treeline will be low
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
1: Low
The avalanche danger rating at treeline will be low
Below Treeline
1: Low
The avalanche danger rating below treeline will be low

Regions: South Rockies.

Freezing levels remain above the mountain tops. Failing cornices could trigger large avalanches running to valley bottoms. Watch out for what's above your head.

Confidence

High

Weather Forecast

FRIDAY: Freezing levels soar to 3500m, sunny, light west ridgetop winds during the day then rise sharply to strong to extreme Friday night. SATURDAY: Freezing levels remain around 2500m, sunny, light westerly ridgetop winds. SUNDAY: Freezing level around 2000m, mix sun and cloud, light westerly ridgetop winds.

Avalanche Summary

No new avalanches were reported in this region on Wednesday.

Snowpack Summary

Cornices are large, fragile, and could trigger deep slab avalanches that run to valley bottoms. Monitoring the overnight freeze of the snow surface is very important during the spring.  If the snow surface does not freeze overnight or if the crust is only a few cm thick, the effect of daytime heating and solar radiation will weaken the snowpack much more quickly than it would if there is a well frozen thick crust.  This is because the crust must first melt before the sun can weaken the snowpack. Deeply buried weak layers in the mid snowpack and near the ground still have the potential to wake up and become active with a rapid warm up. While unlikely, releases on these deeply buried weak layers would result in very large avalanches. Glide cracks are widespread, active, and best avoided. Low elevation and thin snowpack areas have become isothermal, meaning the snowpack is 0 degrees Celsius throughout. An isothermal snowpack is more prone to full depth wet slab avalanches during the heat of the day.

Avalanche Problems

Cornices

If the sun is shining, cornices present a significant hazard. Even if they don't trigger a slab avalanche when they fall onto a slope, they have a nasty habit of running surprisingly long distances.
Pay attention to overhead hazards like cornices. >Cornices become weak with daytime heating, so travel early on exposed slopes. >Give cornices a wide berth when travelling on or below ridges. >

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

Elevations: Alpine, Treeline.

Likelihood: Possible

Expected Size: 3 - 6

Wet Slabs

Avoid steep slopes with an isothermal snowpack during the heat of the day. 
Avoid exposure to overhead avalanche terrain, large avalanches may reach the end of run out zones. >Choose regroup spots carefully. >Avoid slopes with glide cracks. >

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

Elevations: All elevations.

Likelihood: Unlikely

Expected Size: 3 - 6

Loose Wet

Changes can be rapid, sometimes significant change is possible in a matter of minutes, certainly within an hour or two.
Avoid sun exposed slopes when the solar radiation is strong, especially if snow is moist or wet.>Look for signs of surface instabilities such as pinwheeling and point releasing near cliffs. >

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

Elevations: All elevations.

Likelihood: Possible - Likely

Expected Size: 1 - 3