Conditions may change quickly with rain or strong solar input. Be ready to scale back your exposure to avalanche terrain if the surface crust breaks down.
Cautious route-finding will be important at upper elevations as wind slabs may be reactive to human triggering.
Wind slabs may exist in steep, lee terrain features in the alpine and exposed treeline. These slabs will be most reactive where they overlie a slick crust.
Springtime cornices are large and unpredictable. Give them a wide berth when travelling at ridge crest and avoid overhead exposure, especially when the air temperature is warm or solar radiation is strong.
Avoid avalanche terrain if the snowpack becomes wet and unsupportive to your weight. At lower elevations, a poor overnight crust recovery followed by above freezing temperatures and rain may cause wet slab and wet loose avalanches to continue on all aspects.
If the sun comes out on Thursday, wet loose activity can be expected on steep solar aspects at all elevations.
WEDNESDAY NIGHT: Cloudy with flurries in the north of the north, up to 5 cm of accumulation. Partially cloudy in the south. Freezing level dropping to around 500 m. 15-35 km/h northwesterly winds.
THURSDAY: Partially cloudy, isolated flurries. Freezing level rising to 1300 m. 10-30 km/h northwesterly winds.
FRIDAY: Mainly cloudy, flurries in the afternoon. Freezing level rising to 1500 m/ 10-25 km/h southwest winds.
SATURDAY: Partially cloudy with isolated flurries. Freezing level rising to 1600 m. 10-20 km/h southwest winds.
On Tuesday in the north of the region, several size 1-2 natural wind slabs were observed in the alpine. Throughout the region, a widespread wet loose/wet slab avalanche cycle occurred at all elevations up to size 3. The most reactivity was noted on solar aspects.
A widespread wet loose/slab natural avalanche cycle up to size 3 occurred on Monday on all aspects and elevations.
The last persistent slab avalanches observed in the region were during the warm-up on March 23rd and 24th.This layer is expected to become dormant after being tested by significant warming followed by cooling temperatures.
5 to 15 cm of new snow overlies 10-20 cm of denser snow above 2000 m. Southwest winds may form small wind slabs in lee terrain features in the alpine and treeline. A crust or moist snow can be found below the new snow on all aspects below 2500m. Below the crust, the top 10-30 cm of the snowpack is moist.
Several other layers exist in the upper snowpack, that have shown no recent reactivity.
