Despite the lack of avalanche activity over past two days don't forget about the persistent layers in the mid and lower pack. Conservative terrain choices are still advised.
Three persistent weak layers formed in January are down 40-110 cm. Buried sun crusts on steep solar slopes present the greatest concern for triggering, however, weak facets and isolated surface hoar can be found on the same interfaces on shaded aspects.
The weak depth hoar at the bottom of the snowpack inspires little confidence. Multiple parties have remotely triggered large slabs from thin areas in the snowpack. Give careful consideration to the slopes overhead as large avalanches may run well into the runout zone or into lower-angle terrain. Avoid big terrain features and be especially cautious in thin or rocky areas, where triggering is more likely.
Several wet loose avalanches up to size 2 have been reported out of steep solar aspects over the past two days. On Tuesday, there was a deep persistent slab reported on Observation peak and Sunshine patrol reported observing two size 2.5 deep slabs in the surrounding backcountry. .
Surface sun crusts exist to ridgetop on solar aspects and to 2000 m on shady aspects. The middle of the snowpack holds several crust layers that has produced numerous natural slab avalanches over the past 10 days. The base of the snowpack is weak, unconsolidated depth hoar in almost all areas.
Friday - A trough of low pressure over the Alberta Rockies will produce cloudy skies and scattered flurries that will increase through the afternoon. Accumulations in the 1-5 cm range. Ridge-top winds will be light and the freezing levels only expected to rise to 1300 m.
