Abstract

A global sensitivity analysis was conducted on a dynamic water balance model with 19 parameters describing canopy structure, stomatal regulation and soil characteristics, to quantify the importance of vegetation and soil properties in coupled models of hydrology and forest dynamics. Main outputs were total evaporation, as well as a physiological drought index calculated from actual and potential transpiration. Parameter sensitivity was assessed at ten temperate to sub-alpine locations, covering both water-limited and energy-limited sites.Varying parameter values within plausible ranges led to differences of several hundreds of mm/year in predicted long-term evaporation. Root zone storage is the most important parameter at drier stations, whereas canopy and stomatal parameters become more important where soil moisture is less limiting. Physiological drought also depends strongly on root zone properties, while canopy structure only matters at the drier sites. Stomatal sensitivity to dry air substantially contributed to drought stress at the more humid sites.

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