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Technical Note: Reducing the spin-up time of integrated surface water–groundwater models

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Table 1. Skjern River sub-catchment annual water balance for the equilibrium year after the baseline spin-up approach and the hybrid approach using the hydrostatic equilibrium and adjusted pressure head distribution options above the water table
Table 2. Baldry sub-catchment annual water balance for the equilibrium year after the baseline spin-up approach and the hybrid approach with the adjusted pressure head distribution option above the water table
Figure 1. The hybrid spin-up approach consists of three main steps: (1) initial ParFlow.CLM spin-up simulations based an arbitrary DTWT distribution, (2) state updating step by  develop-ing a DTWT function based on percent changes in mean annual DTWT in in
Figure 2. Sub-catchment of the Skjern river basin located in western Denmark (reproduced from Ajami et al., 2014) (left), and Baldry sub-catchment in Australia (right)
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