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A two-parameter annual water balance model was developed for reconstructing annual terrestrial water storage change (ΔTWS) and groundwater storage change (ΔGWS).
Huss, M. Present and future contribution of glacier storage change to runoff from macroscale drainage basins in Europe.
The GRACE-derived terrestrial water storage change (TWSC) provides an unprecedented opportunity to close the terrestrial water budget.
The derived moment approach can be used in ungauged watersheds when neglecting the annual water storage change.
In the ice-cover seasons, the supra-permafrost discharge contribution varied between −20% and 22% of the water storage change.
The storage change in two different groundwater withdrawal scenarios shows gradually declining groundwater storage in both scenarios.
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The model uses precipitation as the principal driver of groundwater storage changes.
Calculated water storage changes in global endorheic regions are distributed through PANGAEA (https://doi.org/10.1594/PANGAEA.895895).org/10.1594/PANGAEA.895895
Storage changes in major lakes and reservoirs are available upon reasonable request to the corresponding author.
The aquifer boundary in brown indicates the regions where the aggregated groundwater storage changes are represented in this study.
The simulated groundwater storage changes for the years 1980 2014 (Blue line) are compared with observations (red icons).
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