Carefully evaluate bigger alpine lines for pockets of wind slab sensitive to human triggering. After Wednesday, the freezing level will start to creep higher.
Recent storm snow is being blown into windslabs in the alpine. Natural activity up to size 1.5 has been observed as recently as Monday in steep alpine terrain below rocky headwalls. Human triggering remains a possibility in steep, unsupported terrain.
Tuesday night: Overcast with isolated flurries bringing around 5 cm of new snow. Moderate southwest winds, strong at ridgetop. Alpine low -5 C. Freezing level around 1000 m.
Wednesday: Broken cloud with isolated flurries bringing up to 5 cm of new snow. Moderate southwest winds. Alpine high -4 C. Freezing level around 1200 m.
Thursday: Broken cloud with isolated flurries bringing a trace of new snow. Moderate west to southwest winds, strong at ridgetop. Alpine high -1 C. Freezing level rising to 1600 m.
Friday: Broken cloud with isolated flurries bringing up to 5 cm of new snow. Moderate west to southwest winds, strong at ridgetop. Alpine high 0 C. Freezing level rising to 1800 m.
On Monday, natural storm slabs up to size 1.5 were observed in steep alpine terrain below cliffy headwalls in the Lizard range. One was triggered by a cornice fall.
Over the weekend, results from control work were also limited to size 1.5. A natural storm cycle occurred Friday size 1.5-2.5.
Thin surface crusts may be found on a variety of aspects and elevations. Wind loaded pockets are forming in lee features in the alpine. After over 1 m of steady snowfall last week, the stout upper snowpack continues to settle in the mild temperatures.
Several crust layers exist in the mid snowpack as a result of previous warming and rain events. These have not been identified as bed surfaces or failure planes in recent avalanche activity.
The bottom 10-20 cm of the snowpack consists of faceted snow and decomposing crusts. Although inherently weak, this basal layer has not been an active avalanche problem in our region since 2019.
