Do Climate Models Need Microphysical and Convective Parameterizations to Generate Accurate Precipitation Fields?
Abstract
Accurately representing surface precipitation is crucial for the operational use of weather and climate models. Presently, global numerical weather prediction (NWP) models struggle to accurately generate precipitation due to their parametrization of unresolved deep convective clouds and, in regions of grid-resolved ascent, inadequate parameterizations of cloud microphysics. Here we bypass these parameterizations with a machine learning model that diagnoses precipitation from 13 ERA5 fields that are easily observed and assimilated, as opposed for example, to fields like rain or cloud liquid water. We train a pair of models; MLERA5 using ERA5 precipitation as the target, and MLIMERG using a satellite based precipitation product. MLERA5 closely reproduces the ERA5 precipitation at all intensities. When evaluated against the satellite dataset, MLIMERG closely matches observations, notably reproducing the diurnal cycle of the satellite product. MLIMERG generally captures extremes better than ERA5 while also reducing ERA5's overproduction of light precipitation. When evaluated against a third ground-and-radar-based dataset, MLIMERG inherits the strengths of the satellite dataset which is superior to ERA5 in the summer months.
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