Avalanche hazard and triggers are influenced by heat these days. If the sun comes out, put loose dry and cornices on your list of things to watch for.
Weather Forecast
A more predictable spring weather pattern seems to be knocking on our door. Tomorrow's high is -8, but the sun will hopefully make an appearance which will spike the temps. Alpine winds will be 40-50km from the west. No snow.
Avalanche Summary
A few loose dry avalanches were noted in the Bow Valley today. In one observed case, the loosed dry triggered a slab mid slope. Probably a 2.5 all said and done.
Snowpack Summary
A cooler day than expected kept the snow dry for the most part. Solar aspects, especially around rocks or trees will probably have a hint of a suncrust by late this afternoon. Speaking of crusts, remember that there is also a buried crust on solar aspects. While not widespread, or thick it can be found on steep terrain. Beyond the predictable crust formation, we still have those pesky windslabs from the last couple of wind events. These range in hardness, but unfortunately seem to be everywhere in the alpine. And of course, we have the lower 2/3's of the snowpack that is still a delicate combo of facets and depth hoar. This is a CRITICAL layer as the spring temps slowly creep up. The buzz around the forecaster's office is the expectation of these waking up easily and suddenly. These avalanches will flow far and fast when they occur.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.