A one‐parameter Budyko model for water balance captures emergent behavior in darwinian hydrologic models

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Understanding the budyko equation (2017, methodology): “Since then, a large number of successful tests of the Budyko equation has been reported based on experimental measurements [5,18,19] and model simulations [14,20].”
A rational performance criterion for hydrological model (2020, background): “…function of Wt: = + +Y W b a W b a W b a2 2t t t t 2 (10) The parameter a represents the propensity for runoff to occur before the soils are fully saturated; the parameter b is the upper bound of storage in the unsaturated zone above the groundwater table (Thomas, 1981; Wang and Tang, 2014).”