Purcells

Wind slabs, cornice fall, or a person could trigger a deeply buried weak layer, creating a surprisingly large avalanche.

We continue to receive reports of natural and skier triggered size 1-2 wind slabs from across the region. The January surface hoar layer remains a major concern, especially in the north Purcells where it has been responsible for several recent large avalanches. On Friday, a snow cat triggered a size 2 persistent slab on a SE aspect near 2300 m. Last Saturday, a size 3 sledder-triggered avalanche occurred in the Gorman Creek riding area near Golden. Around the same time, a size 3.5 skier-triggered persistent slab avalanche occurred a few drainages to the south of Gorman Creek on a north-facing alpine slope. Forecast warming may increase the reactivity of the persistent slab.

Moderate - Timing or intensity of solar radiation is uncertain

A building ridge is expected to bring mainly sunny skies with no precipitation for the next three days. A warm southerly flow causes the freezing level to rise as high as 3000 m.For more details check out https://avalanche.ca/weather.

Reactive wind slabs exist in the lee of ridges and terrain breaks at alpine and treeline elevations. These may be found lower in the start zones than normal due to the high wind speed. A persistent weak layer of surface hoar and facets buried in early January is now typically down 40-90 cm. The layer is slowly getting harder to trigger in many areas. However, reports of whumpfing and some recent large to very large avalanches around Golden indicate this layer is still very much a concern, especially in the north of the region. In general, the lower snowpack below this layer is well settled and strong.