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Assimilating in situ and radar altimetry data into a large scale hydrologic hydrodynamic model for streamflow forecast in the Amazon

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Figure

Fig. 1. Sensitivity tests of DA scheme parameters. Mean changein root-mean-square error (�rms) for the assimilation (line withstars) and validation (line with dots) stream gauges as function ofensemble size (N), precipitation relative error (E) and spatial
Fig. 2. Evaluation of in situ discharge assimilation. Spatial distribution of change in root-mean-square error (�rms) in stream gauges usedfor data assimilation (circles) and validation (squares) considering the assimilation of (a) almost all gauges (Exp
Fig. 3. Discharge derived from in situ observation (blue line), open-loop simulation (black line) and EnKF simulation (red line) at (a) NegroRiver (assimilation site, Exp
Fig. 4. Evaluation of ENVISAT radar altimetry data assimilation. Spatial distribution of change in root-mean-square error (�rms) at (a)altimetry stations used for data assimilation and stream gauges with (b) stage and (c) discharge data used for verification.
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