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Improved large scale hydrological modelling through the assimilation of streamflow and downscaled satellite soil moisture observations

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Figure

Figure 1. Map of the Murrumbidgee River basin and its locationin Australia as part of the Murray–Darling system
Figure 3. PCR-GLOBWB model structure, adapted from Van Beeket al. (2011). Symbols’ definitions are as follows: Precip, pre-cipitation; Evap, evaporation; T , temperature; S1, first soil layer;S2, second soil layer; S3, third soil layer; S4, groundwater reser-voir; Qchannel, total runoff; QDR, direct runoff; QIF, intermediateflow; QBF, baseflow; and Inf, water flow from the river channel tothe groundwater reservoir.
Figure 4. Daily mean precipitation, temperature and reference evapotranspiration for the time period 2007–2010 from the (i) global(0.5◦ × 0.5◦), (ii) downscaled global (0.08◦ × 0.08◦) and (iii) local (0.05◦ × 0.05◦) forcing data sets.
Table 1. Catchment daily mean (µ)/standard deviation (σ) of precipitation (P ), temperature (T ) and reference evapotranspiration (ET) in theMurrumbidgee River basin for 2007–2010.
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