Journal Article

Variations of global and continental water balance components as impacted by climate forcing uncertainty and human water use

Müller Schmied, H, Eisner, S, Song, Q, Adam, L, Reinecke, R, Flörke, M, Kim, H, Oki, T, Fink, G, Portmann, F. T, Riedel, C, Döll, P, Zhang, J

2016

Overview

When assessing global water resources with hydrological models, it is essential to know the methodological uncertainties in the water resources estimates. The study presented here quantifies effects of the uncertainty in the spatial and temporal patterns of meteorological variables on water balance components at the global, continental and grid cell scale by forcing the global hydrological model WaterGAP 2.2 (ISI-MIP 2.1) with five state-of-the-art climate forcing input data-sets. While global precipitation over land during 1971--2000 varies between 103 500 and 111 000 km.sup.3 yr.sup.−1, global river discharge varies between 39 200 and 42 200 km.sup.3 yr.sup.−1 . Temporal trends of global water balance components are strongly affected by the uncertainty in the climate forcing (except human water abstractions), and there is a need for temporal homogenization of climate forcings (in particular WFD/WFDEI). On about 10--20 % of the global land area, change of river discharge between two consecutive 30 year periods was driven more strongly by changes of human water use including dam construction than by changes in precipitation. This number increases towards the end of the 20th century due to intensified human water use and dam construction. The calibration approach of WaterGAP against observed long-term average river discharge reduces the impact of climate forcing uncertainty on estimated river discharge significantly. Different homgeneous climate forcings lead to a variation of Q of only 1.6 % for the 54 % of global land area that are constrained by discharge observations, while estimated renewable water resources in the remaining uncalibrated regions vary by 18.5 %. Uncertainties are especially high in Southeast Asia where Global Runoff Data Centre (GRDC) data availability is very sparse. By sharing already available discharge data, or installing new streamflow gauging stations in such regions, water balance uncertainties could be reduced which would lead to an improved assessment of the world's water resources.

• Publisher: Copernicus GmbH
• Subject: Analysis / Climate / Precipitation (Meteorology) / Streamflow / Water balance (Hydrology) / Water resources / Water use