Abstract
The lack of hydrological data and the low quality of global hydrological models’ output caused by incapability of proper calibration is the main problem when using hydrological models to study the closure of the water balance at river basin scales. Monthly GRACE gravity field solutions can be used to infer water storage variations at river basin scale. However, the estimates are erroneous due to measurement errors, aliasing effects, and limited spatial resolution, which makes it difficult to verify and improve the hydrological models.
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