Both wind slabs and deep persistent slab avalanches remain human triggerable, especially on steep wind loaded features immediately lee of ridge crest. See the Avalanche Summary for some great information about a near miss with a deep avalanche on Sunday.
Wind slabs have formed above a widespread crust, natural activity has slowed down, but human triggering remains possible. Potentially deep wind slabs can likely be found near ridge crest.
This layer produced a very large avalanche on Sunday, more details here. When considering terrain you need to be thinking about the potential for deep avalanches. The most likely trigger points are thin rocky areas near ridge crest. Rock outcroppings in exposed terrain should be avoided.
Aside from a few bouts of potentially strong wind, we continue to be in a rather benign weather pattern which is expected to be with us for the foreseeable future.
MONDAY NIGHT: Freezing level at valley bottom, moderate west/southwest wind, no significant precipitation expected.
TUESDAY: Broken cloud cover, freezing level rising to around 1500 m in the afternoon, moderate to strong west/southwest wind, 1 to 5 cm of snow possible.
WEDNESDAY: Broken cloud cover, freezing level near valley bottom, light variable wind, trace of precipitation possible.
THURSDAY: Scattered cloud cover, freezing level rising to around 1500 m in the afternoon, moderate to strong southwest wind, trace of precipitation possible.
Over the weekend numerous natural, human triggered and control work induced avalanches to size 2 were observed, there is a great MIN that serves as an example of this kind of activity here.
There was also a bigger avalanche reported in this MIN on February 9th (check out the photos, they're humbling). The very large avalanche ran on a north facing feature at 2400 m and was triggered by a snowmobile. The group was using excellent travel protocol and thankfully no one was hurt. 10 or so climbs had been made in the same area in the days leading up to this avalanche without incident and that's what makes dealing with persistent slabs so tough.
Before the above avalanche, the last avalanche cycle to include persistent slabs was during the first weekend in February when some large (size 2.5) deep persistent slab avalanches in the Elk Valley (see photos in this MIN report) ran. These were similar to avalanches in that area from mid-January, which suggests the deep persistent slab problem may resurface during stormy periods.
5 to 15 cm of storm snow from the Friday Night/Saturday storm adds to the variable amounts of wind affected snow that sits above a widespread rain crust that exists up to roughly 2100 m. The storm snow has been formed into slabs by wind from a variety of directions. The Elk Valley has 5-20 cm of snow above the crust and the eastern slopes have 15-35 cm above the crust. There have been observations of surface hoar forming in the Elk Valley previous to Friday Night's storm, check that out here. A well consolidated mid-pack overlies generally weak basal facets, that may be possible to trigger in isolated shallow rocky start zones.
