Earth System Dynamics· 2014Q1
Global modeling of withdrawal, allocation and consumptive use of surface water and groundwater resources
- 881citations
- Q1SCImago
- 2014year
Short summary
A new coupled global hydrological and water demand model dynamically simulates daily water withdrawal and consumptive use from 1979-2010, distinguishing between surface and groundwater, and showing a global increase in both, with groundwater use rising faster since the 1990s.
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Key points
- A new global model couples hydrological processes with water demand to simulate daily water withdrawal and use (1979-2010).
- The model distinguishes between surface water and groundwater withdrawals and includes dynamic irrigation and reservoir operations.
- Simulated withdrawals generally agree with national and subnational statistics.
- Global surface and groundwater use increased consistently, with groundwater use showing a more rapid rise since the 1990s.
- Human water use significantly alters terrestrial water storage variability, especially in regulated and irrigated basins.
AI-generated from the title and abstract; the full text is not read.
Abstract
Abstract. To sustain growing food demand and increasing standard of living, global water withdrawal and consumptive water use have been increasing rapidly. To analyze the human perturbation on water resources consistently over large scales, a number of macro-scale hydrological models (MHMs) have been developed in recent decades. However, few models consider the interaction between terrestrial water fluxes, and human activities and associated water use, and even fewer models distinguish water use from surface water and groundwater resources. Here, we couple a global water demand model with a global hydrological model and dynamically simulate daily water withdrawal and consumptive water use over the period 1979–2010, using two re-analysis products: ERA-Interim and MERRA. We explicitly take into account the mutual feedback between supply and demand, and implement a newly developed water allocation scheme to distinguish surface water and groundwater use. Moreover, we include a new irrigation scheme, which works dynamically with a daily surface and soil water balance, and incorporate the newly available extensive Global Reservoir and Dams data set (GRanD). Simulated surface water and groundwater withdrawals generally show good agreement with reported national and subnational statistics. The results show a consistent increase in both surface water and groundwater use worldwide, with a more rapid increase in groundwater use since the 1990s. Human impacts on terrestrial water storage (TWS) signals are evident, altering the seasonal and interannual variability. This alteration is particularly large over heavily regulated basins such as the Colorado and the Columbia, and over the major irrigated basins such as the Mississippi, the Indus, and the Ganges. Including human water use and associated reservoir operations generally improves the correlation of simulated TWS anomalies with those of the GRACE observations.
The authors' abstract, as published at the source. Earth System Dynamics, 2014 · DOI ↗
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