Wet Snow is a complex problem, as it can be very predictable and yet unpredictable at the same time. What does this mean? We know that the sun will rise and warm the snow surface, starting the melting process once again and create more wet avalanches as the day wears on. What we cannot predict is the exact extent or timing of the avalanche activity. We just know, that if the slope is wet and unconsolidated, we don't want to be on or underneath it. The Wet Snow Avalanche Problem covers two types of avalanches:

Wet Loose Avalanches - These typically occur within layers of wet snow near the surface caused by warming temperatures and strong sunshine. As the snow becomes wet, the upper surface layers become unconsolidated as the bonds between the snow grains lose their cohesion. They start at a point and typically fan out as they move downhill. These avalanches can entrain a lot of snow, especially in a tight rock-lined chute or in sustained steep terrain. The first sign of wet loose avalanches is usually rollerballs or pinwheels. Today, these avalanches can happen naturally or be human-triggered.

Wet Slab Avalanches - This is a tough one; we haven't seen any wet slab avalanche activity in the backcountry up to this point. However, now on our third night with temperatures above freezing, I wouldn't be surprised to hear some wet slab avalanche activity. Basically, the way this works is your slab (stronger snow) fails on wet saturated snow grains below in the snowpack somewhere. Meltwater can also saturate a layer of snow, and that becomes the weak layer releasing the slab of stronger snow above.

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If you want to dive deeper into Wet Slab Avalanches check out this paper on this topic HERE.