Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterFeb 25th, 2021–Feb 26th, 2021
South Columbia.
New snow and wind will mean that storm slabs are to be expected, and will likely be reactive to human triggering in many areas.
The potential exists to trigger deeper weak layers, resulting in large avalanches. Choose conservative terrain.
THURSDAY NIGHT - Flurries, 10-15 cm / moderate to strong west wind / alpine low temperature near -10
FRIDAY - Mainy cloudy with flurries, 5 cm / moderate northwest wind / alpine high temperature near -10
SATURDAY - A mix of sun and cloud with a few flurries / moderate west wind / alpine high temperature near -12
SUNDAY - Mainly cloudy with scattered flurries, 5 cm / moderate to strong southwest wind / alpine high temperature near -6 / freezing level 1500 m
On Wednesday, there were a few reports of size 1.5-2 natural and human-triggered storm slab avalanches in the alpine and at treeline, on all aspects.
On Tuesday, there were several reports of natural, human and explosives-triggered avalanches up to size 3, though most were in the size 1-2 range.
During the storm last weekend and into Monday, there was a widespread natural and explosives-triggered avalanche cycle, with avalanches ranging from size 2-4, reported in the Selkirks in the northern part of the region.
The Monashees had surprisingly limited activity up to size 2 in the same time period. Reports from Monday described size 1-2 natural, explosive, and human-triggered avalanches, as well as one report of a size 3 natural cornice triggered avalanche.
There have been a few reports from the south of the region of sporadic persistent slab avalanches failing on the late January persistent weak layer. These have been around size 2, human-triggered, and out of steep, cliffy, unsupported terrain around treeline.
10-15 cm of new snow is expected on Thursday night with another 5 cm on Friday. This will add to the 60-100 cm of recent storm snow. Deep wind deposits may be found in lee terrain features in the alpine and open treeline areas, and will likely remain reactive to human triggers. All of this new snow sits over weak, faceted snow from the recent cold snap.
There is now 70-120 cm of snow above the late January persistent weak layer which is composed of surface hoar in sheltered areas in the trees and/ or a crust on steep solar aspects. Very isolated activity on this layer has been observed recently, usually skier triggered in steep, cliffy, unsupported terrain around treeline in the south of the region.