Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Jan 25th, 2017–Jan 26th, 2017

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

Regions

Glacier.

Weather Forecast

Unfortunately the ridge of high pressure will continue to block hope of any significant snow this week. Today expect mainly cloudy with no precipitation, an alpine high of -10*C and light winds. Thurs and Friday will be cloudy and although we may see some isolated flurries, they will only bring a trace of snow.

Snowpack Summary

~40cm of snow from last weeks storm is settling and is generally bonding. In some areas it overlies surface hoar and will be more reactive. Cooler temps are helping to soften the upper slab, improving snow quality. Recent snowpack tests generally indicate that the snowpack is stubborn to triggering, however it is weakest a low elevations.

Avalanche Summary

Recent natural avalanche activity has been limited to steep unskiable terrain such as off Mt Macdonald. However, there have been size 2.5 avalanches observed from this type of terrain regularly with avalanches running onto fans. Sluffing when skiing/riding steep terrain has also been observed.

Confidence

Wind effect is extremely variable

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.