Although most of the snow seemed rather well-behaved, the main problem is the lingering wind slabs from the strong southerly winds for the past couple days. I expected to see more wind slabs along the upper elevation ridges but it appears like the wind was so strong that it just scoured all the upper elevation terrain and most of the wind-slabbed snow was down lower on the slope and even in some of the upper elevation drainage bottoms--well down off the ridges. It was a tricky wind pattern and the wind seemed to swirl around a lot so the loading was on a variety of aspects.

Luckily, most of the wind slabs were settled out and we could not get any of them to crack. They are more tricky to recognize than usual because the inch of new snow hides the texture.

Very little activity occurred at the ski resorts today with the exception of one significant result from one of the Park City areas that typically loads with south winds. The avalanche was triggered by a controlled cornice fall. So they are out there, just a bit stubborn.

The lower elevation snow is still moist and isothermal. We noticed a couple small, wet sluffs on steep slopes but nothing major. I suspect wet activity will remain fairly well behaved until we get another big warm up or low elevation rain again.