Carefully assess steep lines for wind slab and limit exposure to slopes with cornices above.
5-15 cm of new snow and shifting winds may have formed small pockets of wind slabs on a range of aspects in exposed areas.
Use caution entering steep, lee terrain features below ridges. The snow could slide easily where it rests on a hard melt-freeze crust.
Cornices are large this time of year and were likely weakened by recent cold temperatures. Exposure to cornices should be minimized, especially during periods of warm temperatures or strong sun. Give them a wide berth when you are travelling on ridge lines and avoid overhead exposure to large cornices.
THURSDAY NIGHT: High cloud increasing. Light westerly winds. Freezing level remains elevated at around 1300 m.
FRIDAY: Increasing cloud cover with light flurries in the afternoon. Light southwesterly winds. Freezing level remaining steady at 1400 m. Treeline temperatures around -1 C.
SATURDAY: Cloudy with snowfall, 5-10 cm of accumulation. Moderate to strong southerly winds. Freezing level around 1400 m. Treeline temperatures around -2 C.
SUNDAY: Cloudy with flurries, up to 5 cm of accumulation. Moderate to strong southwesterly winds. Freezing level 1000 m. Treeline temperatures around -4 C.
A small skier-triggered wind slab was reported near Terrace on Wednesday (size 1). This avalanche occurred on a convex roll in the alpine and failed on slick melt-freeze crust.
A few natural wind slab releases were observed in the Bear Pass area on Tuesday afternoon. These reached size 2 (large) and were limited to steep, wind-loaded features in the alpine.
Looking forward to Friday, small but reactive wind slabs may exist in lee features in the alpine. Winds have varied in direction, so watch for wind slabs on all aspects.
5-15 cm of new snow buried heavily wind-affected surfaces in open areas, the product of strong outflow wind early last week. In open areas, this new snow has been redistributed by easterly winds into small pockets of wind slab in lee areas. A crust will likely be found on steep solar aspects from warm temperatures and sun yesterday. Below 1200 m, a more widespread crust exists at or near the surface. Above 1200 m, 40 to 80 cm of settled storm snow is well bonded to another hard melt-freeze crust from late March.
