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Validation of terrestrial water storage variations as simulated by different global numerical models with GRACE satellite observations

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Figure

Table 1. Overview of the main characteristics of the four numerical models particularly considered in this study.
Figure 1. Locations of 31 globally distributed basins from the sim-ulated topological networks (STN-30p) with underlying Köppen–Geiger climate zones
Figure 3. Phase differences for the annual signal of four hydrological model realizations with GRACE-based TWS observations.
Figure 4. Variance of GRACE-based TWS observations that is explained by TWS as simulated in four hydrological model realizations.
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