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Comparing the ensemble and extended Kalman filters for in situ soil moisture assimilation with contrasting conditions

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Figure

Figure 1. The soil moisture fluxes for the three-layer version ofISBA. The variables Pg, Eg and Etr represent the precipitation, baresoil evaporation and transpiration respectively
Table 1. Table summarizing the different methods. “Cov” stands forcovariance matrix.
Table 2. Table showing the experimental set-up for the synthetic and real DA experiments.
Figure 2. Locations of the 12 sites used for the experiments (redcrosses), selected from the SMOSMANIA network
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