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James F. Booth, Catherine M. Naud, and Jeff Willison

precipitation in ERAI cannot yet be compared with observations. With the recently released NASA Global Precipitation Measurement (GPM; Skofronick-Jackson et al. 2017 ) radar–microwave radiometer combined product ( Grecu et al. 2016 ), this may change in the near future. However, the work presented here focused on the relative similarities and differences in the precipitation generated by the convection schemes for ERAI, the GCMs, and WRF and examined if the differences affected the link between

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