Three things to note: 1) Strong northeast wind has formed wind slabs on atypical slopes. 2) Buried weak layers remain possible to trigger. 3) Sunny skies and a warming trend could start to weaken sun-exposed slopes and cornices.
Wind slabs were recently formed from strong northeast wind. This wind direction is atypical, so you may find wind slabs in terrain features that don't typically have them. This snow will further load deeper layers, meaning there is potential for step-down avalanche activity.
Around 60 to 80 cm of snow overlies a weak layer of surface hoar. This layer has been most problematic on northwest to northeast aspects between 1600 m and 2300 m, but it may exist on all aspects and at all elevations. Assess the layer prior to committing to avalanche terrain or adopt a conservative mindset to avoid the problem.
The snowpack will undergo a rapid change as the freezing level rises and clear skies prevail. For Sunday, loose wet avalanche activity is most likely during the heat of the day on sun-exposed slopes. Cornices will also weaken with the warming trend.
SATURDAY NIGHT: Clear skies, light to moderate east wind, alpine temperature -14 C.
SUNDAY: Clear skies, light northeast wind, alpine temperature -5 C, freezing level rising to 1000 m.
MONDAY: Clear skies, light northeast wind, alpine temperature -4 C, freezing level 1500 m.
TUESDAY: Clear skies, light northeast wind, alpine temperature -1 C, freezing level 1900 m.
Many wind slab avalanches were triggered on Saturday. They were most often on southerly aspects and at treeline and alpine elevations. They were rated as small (size 1.5).
Widespread avalanche activity is starting to quiet down on the surface hoar layer described in the Snowpack Summary. Over the past two weeks, small to large (size 1 to 2) avalanches have released on this surface hoar layer. They have most often released between 1800 and 2300 m on northwest to east aspects.
A major warming trend is forecast for the coming days, which could rapidly weaken the snowpack and cornices.
The upper snowpack is relatively complex. Strong northeast wind has formed wind slabs in south to southwest terrain features near ridges. These aspects don't typically have wind slab problems. A few different layers of surface hoar and melt-freeze crust exist, which have recently acted as sliding layers. One such layer buried about a week ago may be found about 20 to 40 cm deep. The most widespread layer was buried late February and is now buried 60 to 80 cm. This layer is most commonly found in open trees (e.g. in this MIN) or sheltered terrain around the upper part of below treeline, treeline, and lower alpine elevations. This layer may only remain a concern in the north and east parts of the region.
The remainder of the snowpack is strong and well-settled.
