Kootenay Boundary

Snowpack and avalanche observations are becoming scarce. If you've been in the backcountry, please tell us what you've seen here on the Mountain Information Network.

Fair - Timing or intensity of solar radiation is uncertain

A ridge of high pressure moves over the interior on Tuesday and should be the dominant feature for the rest of the week. On Tuesday, a mix of sun and cloud is expected with light alpine winds and freezing levels reaching around 1800m in the afternoon. Isolated convective flurries are possible. Mostly sunny conditions with light alpine winds are expected for Wednesday and Thursday. Freezing levels are expected to reach around 2000m on Wednesday and 2200m on Thursday.

Observations are becoming more limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Sunday, natural and human-triggered wet sluffing was reported. This was limited to size 1 and was sliding on the late-March crust layer. On Saturday, explosives triggered small wind slabs and thin storm slabs that ran on the crust. With freezing levels rising and lots of sun expected on Tuesday, lots of natural sluffing is expected from steep sun-exposed slopes. Cornices will become weaker than they have been for the last week and may fail naturally. Wind slabs in the alpine are expected to be sensitive to human-triggering. Reverse loading may have occurred and wind slabs should be expected in leeward features on all aspects.

Melt-freeze surface conditions exist on sun-exposed slopes. On shaded slopes, 10-20cm of recent snow overlies a thick supportive melt-freeze crust. At higher elevations these accumulations have been blown around by variable winds and thin wind slabs may exist on a variety of aspects. The mid-March crust/facet complex is buried around 50cm below the surface. This layer is generally considered dormant while the cooler temperatures prevail. The mid and lower snowpack are strong and well settled.