A three-stage calibration improves WRF-Hydro streamflow skill for eastern Canada and produces 1990-2100 discharge projections with reduced inter-model spread and confirmation of earlier spring peaks.
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A seasonal to decadal calibration of 1990-2100 eastern Canadian freshwater discharge simulations by observations, data models, and neural networks
A three-stage calibration improves WRF-Hydro streamflow skill for eastern Canada and produces 1990-2100 discharge projections with reduced inter-model spread and confirmation of earlier spring peaks.