Green doesn't necessarily mean go. During periods of intense sun avalanche danger may be higher on steep solar aspects. Consider your exposure to cornices as you choose your objectives, they become weaker when the sun is beating down on them.
Weather Forecast
Today will be mostly sunny with a high of -4'C and light to moderate westerly winds. On Thursday there will be increasing cloud, as a weak system passes through the province. We may see a trace of new snow. On Friday we will see a mix of sun and cloud as the ridge of high pressure rebuilds.
Snowpack Summary
Below 1900m a few cm's of snow sits on a hard crust. 15-20cm of snow sit on the Feb 18 surface hoar layer, which exists up to 2200m. The Feb 14 crust is down 20-25 and is up to 10cm thick. Variable wind effect, with pockets of thin hard slab, exists in exposed areas at treeline and above. Persistent weak layers down 1-1.5m are stubborn to trigger.
Avalanche Summary
Recent natural avalanches have been primarily solar triggered. Strong solar has triggered loose wet avalanches, or caused cornices to fail sometimes triggering deep slabs. Small pockets of windslab have been triggered by skiers, which is primarily a concern on exposed slopes where the consequences are high (ie steep faces or over cliffs).
Problems
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.