The combined use of ground and remote sensing data in hydrological modeling applications significantly improve models’ performance and provide decision makers with timely, objective, accurate, and actionable information to improve water management and strengthen food security. This is especially the case for data scarce environments in which the lack of ground-based observations hinders hydrological models’ predictability capacity. Indeed, remote sensing products facilitate routine monitoring of hydrological processes, water resources, deficits and extremes. The incorporation of satellite-derived hydrological variables during a calibration processes add constraints to the model parameters, which results in reduced model uncertainties and a reduced number of equifinal solutions.
This study attempts to test the improvement of the semi distributed Soil & Water Assessment Tool (SWAT) model’s performance, expressed as the goodness-of-fit between observed and simulated streamflow, after assimilating the Integrated Multi-satellitE Retrievals for GPM (IMERG) precipitation products and evapotranspiration time series derived from the Moderate Resolution Imaging Spectroradiometer (MODIS). At the same time this research focuses on analyzing the differences in model parameters sensitivity between a streamflow-based calibration approach and a combined streamflow and satellite-derived evapotranspiration-based calibration approach.
This research comprises the following steps: First, the model is run using ground data as model inputs, followed by a streamflow-based calibration process. Second, the optimized model is recalibrated and rerun after replacing the ground precipitation inputs by satellite-derived precipitation data that was resampled at subbasin level. Finally, a multi-objective calibration approach will include different sources of observed data, discharge (ground) and evapotranspiration (satellite), as an attempt to add constraints to model parameters and to reduce model uncertainties and the number of equifinal solutions.
Preliminary results showed that SWAT model performance, based on the efficiency coefficient NSE, significantly improved after incorporating remote sensed precipitation data. The initial NSE value after the streamflow-based calibration approach was 0.13, but reached to 0.51 when the model was run and fully calibrated using satellite-derived data. It is expected that the multi-objective calibration approach highlights differences on the optimized model parameter values between the two calibration approaches.