Diffusion downscaling trained on MESACLIP data applied to CESM2 indicates SAI nearly halves the CONUS-average increase in yearly maximum precipitation.
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Precipitation diffusion downscaling and application to out-of-distribution simulations with and without stratospheric aerosol injection
Diffusion downscaling trained on MESACLIP data applied to CESM2 indicates SAI nearly halves the CONUS-average increase in yearly maximum precipitation.