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Temporal variation of soil moisture over the Wuding River basin assessed with an eco hydrological model, in situ observations and remote sensing

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Figure

Fig. 1. The normal distribution for the two-tailed hypothesis test in Mann-Kendall method.Fig
Fig. 3. The yearly evolution (upper two panels) of and the correlation (lower three panels) among relative SM simulated by VIP, retrievedfrom remote sensing TUW data and observation at Suide and Yulin.
Fig. 5. The simulated averaged annual evapotranspiration (ET) and the observed ET which is  The simulated averaged annual and the observed ET whichis the difference between the observed annual precipitation and dis-charge based on water balance (wb) of the 9 sub-catchments of theWuding River basin in 2000.
Fig. 6. Seasonal cycle (left panel) of monthly mean SM in the 0–2 cm surface layer (Fig
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