To me it seems to come down to how well the snowpack is draining. If water melting at the surface is able to run to the ground, then it's relatively straightforward to grasp the risk of climax slides and where they're likely to occur (typically on smooth, sloped rock such as the entirety of the terrain out the lower gate at Alpental). If that water isn't percolating fully through the snowpack, it may be lubricating a buried weak layer which dramatically increases the risk of wet slab avalanches. Those are the kind that terrify me - loose wet slides are predictable and while not entirely avoidable, usually manageable with ski cutting and smart terrain selection. Wet slabs can release above you and bring an incredibly massive amount of snow down in a much quicker fashion than a wet loose slide.
That said, a wet loose slide can entrain a large amount of snow and run for a very long distance. You need to be aware of those below you as well as attentive to any terrain traps when the risk of wet loose avalanches is present.
How can you determine how well the snowpack is draining? That I don't have a great answer for as digging a snowpit to the ground is exhausting and time-consuming at this point in the year.
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