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Modeling subsurface hydrology in floodplains

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Figure

Figure 1. Structure of HaughFlow, the model created for this study. Box 1 shows the calculation of the water table or the extent of the phreatic zone, with riverstage records as input to the Boussinesq equation and the water table height feeding into the v
Figure 2. Map (modified from Lamontagne et al., 2015) showing the locations of the study sites along the Namoi river,within the Murray-Darling catchment, in south-east Australia.
Figure 3. Plots of the surface and lateral inputs to the model. (a) A time series of precipitation minus the actual evapotranspiration at Old Mollee 50 m
Figure 4. (a and b) Uncoupled 2014 Yarral East 40 m calibration, and (c and d) coupled 2013 Yarral East 290 m calibration
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