High overnight freezing levels and rain are expected to make the snowpack weak at lower elevations, with new wind slabs potentially forming up high.
Look for low angle, higher elevation objectives without overhead cornices. Plan your access and egress route carefully.
Wind slabs may exist in steep, lee terrain features in the high alpine. These wind slabs will be most reactive where they overlie a slick crust.
Warm temperatures may cause cornices to become weak. Cornice failures are dangerous on their own, but also have the potential to trigger larger avalanches on the slopes below.
A weak layer may be found around 50 to 100 cm deep. The layer is most likely to be triggered between 2000 and 2300 m, on all aspects. The likelihood of triggering this layer is decreasing, but the consequence of doing so would be high.
Avoid exposure to large open slopes during intense rain, sun, or warming. High freezing levels and rain has triggered large wet slab avalanches on steep, open terrain features at treeline and below, especially where the snowpack sits over smooth rock slabs or grassy slopes.
Wet loose avalanche activity is expected on steep slopes below the freezing line where the surface snow is wet and unsupportive to your weight.
SUNDAY NIGHT: Cloudy with light flurries. Alpine temperature around 0 C. Ridge winds 15-35km/h southwest. Freezing level 1900m.
MONDAY: Mainly cloudy with flurries, 5 cm of accumulation above the rain-snow line. Alpine temperature around 0 C. Ridge winds 15-30 km/h southwest. Freezing level 2200 m.
TUESDAY: Mainly sunny. Alpine high of 3 C. Ridge winds 15-30 km/h northwest. Freezing level rising to 2000 m.
WEDNESDAY: Mainly cloudy with rain/snow, 5-10 cm of accumulation above the rain/snow line. Alpine temperatures around -3 C. Ridge winds 15-40 km/h southwest. Freezing level rising to 1800 m.
Several small (size 1-1.5) skier-triggered wind slabs occurred on Friday and Saturday. Several small (size 1) wet loose avalanches were observed on Saturday as a result of warm temperatures and solar radiation.
The last persistent slab avalanches observed in the region were during the warm-up on March 23rd and 24th. Several large (size 2-3) persistent slab avalanches occurred. These slabs were 70 to 150 cm deep and occurred on all aspects from 2100-2300 m.
5 to 15 cm of recent snow and southwest winds may have formed small wind slabs in lee terrain features in the high alpine. A refrozen crust can be found below the new snow on all aspects to at least 2300m. This crust is expected to break down throughout the day with rain and warm temperatures. Below the crust, the top 10-30 cm of the snowpack is moist. At low elevations, the snowpack may become wet and isothermal.
A weak layer may be found around 50 to 100 cm deep. The layer consists of surface hoar crystals in treeline terrain on northerly aspects or weak faceted grains above a hard melt-freeze crust on sun-exposed slopes (i.e., east, south, west). It has been reactive between 1800 and 2300 m but given the recent rain, it is most likely to be triggered between 2000 and 2300 m. It should still be treated as suspect if you find it in your riding area.
The remainder of the snowpack is well-bonded.
