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Additional data like Leaf Area Index (LAI) and Net Primary Productivity (NPP) are also used.

               Static  data  sources,  including  soil  moisture,  digital  elevation,  and  landcover,  were  also

               incorporated. The availability of measured discharge and precipitation data for the Zambezi

               basin provided a basis for extensive validation of the water accounting model. All datasets
               used for Zambezi basin, cover the period from 2003 to 2023. This is because, remote sensing-

               based actual ET was only available from 2003, and 2023 was the last full year for which data

               was  available  when  the  generated  discharge  data  for  the  water  accounting  model  was
               developed. However, with more recent data are now being available, this is easily updated. A

               comprehensive table of these data sources is available in Annex 3.1.











































               Figure 2. Volta River Basin in West Africa (Dembélé et al., 2023.)



               3.4 Running the Water Accounting Plus Model for the Volta Basin


               The Volta SIWA+ model was run for the period 2003-2021 with the first couple of years used

               for “model warm-up”.  Outputs from the VegET model of (Akpoti et al., 2024) served as input
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