What models have been struggling with (obviously besides surface temps) is the convective nature of the precipitation.
With these waves being so subtle, large scale forcing has been pretty weak. That said, there's just enough instability/moisture/covergence in the lower levels (below 700mb) in combination with the weak lift to generate intense but intermittent areas of precipitation.
Yes, worst case, such a setup can be catastrophic for narrow corridors that end up under the most persistent/stationary banding. However, it can also be a real feast or famine as far as how widespread the impacts and amounts are.