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P. C. D. Milly and Krista A. Dunne

way that such checking can be done. In the past, hydrologically relevant climate-model outputs other than precipitation and near-surface air temperature were not readily accessible outside the climate-modeling centers; this is no longer the case. We therefore recommend also that consideration be given henceforth to the direct use of radiation outputs from climate models when hydrologic adjustment is performed. Because radiative fluxes constitute the major source term in the surface energy

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