The new snow was very light, and did not receive any wind affect overnight. I saw no evidence of natural avalanches. I believe the low density snow was not enough to become a trigger on the sensitive wind slabs that I observed Sunday. The bad news is that it has covered up the wind slabs, making them harder to recognize. I did not venture into steep terrain that I thought my be windloaded today, as I felt it would be too risky, so unfortunately I can't comment on the existing instability and it's rate of change. I would expect that since it has remained below freezing all day above 8000 feet, and cloudy, that the wind slabs will still be potentially sensitive, but inevitably less so than Sunday. The vexing question is, of course, "how much less?" I can't answer that question, but I can say that it is important to ask the question still, and not just march up steep terrain because it's April. Until it warms up again, there is plenty of poorly bonded slab material from Sunday to make me very cautious.