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Leah S. Campbell and W. James Steenburgh

the highest resolution within the boundary layer, and a 5000-m-deep Rayleigh damping layer at the upper boundary. We performed a series of sensitivity studies using various microphysics, radiation, and planetary boundary layer and surface layer schemes (not shown). Based on the combination that best captured the observed precipitation distribution and taking into account microphysics and planetary boundary layer/surface layer sensitivity studies for lake-effect events presented in Reeves and

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