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Impact of remotely sensed soil moisture and precipitation on soil moisture prediction in a data assimilation system with the JULES land surface model

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Figure

Figure 1. TAMSATv2.0 and v3.0 yearly cumulative rainfall averaged over the 6 years in our experiments (2009–2014).
Figure 3. Number of available days of ESA CCI soil moisture ob-servations in the experiment period (2009–2014) out of a maximumof 2190 days.
Figure 4. Soil moisture data assimilation results for a northern Ghana grid cell using TAMSAT v3.0 driving data
Figure 5. As Fig. 4, except for southern Ghana.
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