Wind slabs developing and likely an issue in and around terrain features and on the lee side of major ridges.. Stiffened and recently built-out cornices also something to be wary of along the ridges.

I noticed a widespread shallowly buried persistent weak layer at the Jan/Feb interface. Main concern here are sugary faceted grains formed near the surface during the cold early February high pressure system, but a capping rime-crust, graupel and surface hoar all add to the mix... The problem with spacial variability comes when you find constants, or less variation. Weak layers with the same properties widespread across a slope probably means avalanches will be more likely when a slab matures.

The existing snow structure is not very good either, with a currently dormant weak layer from early January consisting of fist-hard faceted snow.