YSU and ACM2 are generally characterized by warmer and drier daytime PBLs, which are more consistent with observations, while the MYJ scheme’s purely local treatment of larger-scale eddies prevents the PBL from mixing as deeply to produce cooler and moister conditions. Similarly, Gibbs et al. (2011) find that the nonlocal YSU scheme and the hybrid local–nonlocal ACM2 scheme produces a drier PBL in a dry convective boundary layer (CBL) than the local MYJ scheme, with YSU and ACM2 better depicting the observed PBL than MYJ.