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Sobol Global Sensitivity Analysis of a Coupled Surface/Subsurface Water Flow and Reactive Solute Transfer Model on a Real Hillslope.

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Academic year: 2021

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Figure 1. Example of mixing subroutine activated by an incoming surface runoff: If a surface cell is ponded, solute concentration is set equal between the surface water and the first numerical layer.
Figure 3. The 4 August 2004 rainfall event. The dotted horizontal line represents the mean saturated hydraulic conductivity of the vineyard soil.
Table 1. Input probability density functions for the model inputs. LN is lognormal, N is normal, T is triangular, and U is uniform.
Table 2 summarizes the different analyses carried out for the study. The methods from [ 51 , 52 ] are used to determine, respectively, the first order and total Sobol indices, and the first order and second order Sobol indices
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