WRF-Hydro simulations are configured with a 1-km land surface model, Noah-MP, and terrain routing grid run at 250 m. Subsurface, surface, and channel routing are turned on in the model to simulate runoff, streamflow, and other processes. Neither lakes and reservoirs nor anthropogenic impacts are explicitly accounted for in these model runs such that the model results produced are fully “unregulated” flow responses. Baseline WRF-Hydro model runs are forced with bias-corrected 4-km convection-permitting WRF simulations (CONUS404) to perform calibration at 17 USGS stream gages from 2013–2018 and select optimal values of basin parameters, which are then transferred to hydrologically similar basins during the regionalization process. After two simulations are run using only CONUS404–the first being a spin-up run from 1999–2004, and the second being a baseline run from 1999–2021–WRF-Hydro is run from 2019–2020 using 36-ensemble members from WRF-WxMod to simulate the effects of seeding on the days during which seeding occurred. Changes to snowpack and streamflow are evaluated basin-wide to understand how cloud seeding alters precipitation and thus water resources in Wyoming.

