Avalanche Forecast

High -

Sunday night: Cloudy with clear periods and isolated flurries with a trace of new snow. Light to moderate southwest winds.Monday: Mainly cloudy with isolated flurries and a trace of new snow. Light southwest winds, increasing overnight. Alpine high temperatures around -16. Tuesday: Cloudy with scattered flurries bringing around 5 cm of new snow, continuing overnight. Light southwest winds, increasing to strong in the alpine. Alpine high temperatures around -11.Wednesday: Cloudy with continuing isolated flurries and a trace of new snow, with new snow totals of up to 10 cm. Flurries continuing overnight. Alpine high temperatures around -10.

A social media post from the Marten area of Elk Valley on Thursday describes touchy persistent slab conditions, with lots of smaller slabs releasing over the mid-January surface hoar layer. Check out the post here. Of note is the fact that this area was previously untracked, leaving the mid-January layer undisturbed. This is something to bear in mind as dry conditions persist and the motivation to step out of well-traveled terrain increases. Areas where this layer is undisturbed are far more likely to hold reactive persistent slabs.

Above 1700 m, 25 to 35 cm of recent snow overlies a variety of surfaces, including feathery surface hoar crystals in shaded and sheltered areas, wind-affected snow in exposed terrain, and a melt-freeze crust on southerly aspects. Recent winds continue to redistribute loose snow and develop wind slabs. Below 1700 m, expect to find around 5-10 cm of low-density snow on a melt-freeze crust.The mid-January layer of surface hoar or a crust is buried around 35 to 45 cm deep. The surface hoar is found on shaded and sheltered slopes and is most prominent between 1600 m and 1900 m but has been found up to 2200 m. The melt-freeze crust is found on south aspects at all elevations. This layer is the subject of our Special Public Avalanche Warning. A social media post from the Elk Valley Snow Shepherds from Wednesday does a great job of highlighting the issue. Check the link here.The middle of the snowpack is generally consolidated. The bottom half of the snowpack is unconsolidated and composed of weak and sugary faceted grains. The basal snowpack is becoming even weaker under prolonged cold temperatures, especially in thin snowpack areas.