Abstract
The effects of climate instability on water resources for irrigation and drinking are less apparently dramatic than sea-level rise and storm surges, but just as sinister. According to experts, there are already a billion individuals dependent upon groundwater sources that are “simply not there as renewable-water supplies.”1 Now planetary warming, in part caused by anthropogenic increases in CO2, is altering precipitation patterns; increasing surface water temperatures, pollution, and atmospheric water-vapor content; and reducing ice- and snowpack, groundwater-recharge rates, and soil moisture. Rising sea levels may also cause saltwater intrusion into coastal groundwater aquifers. At the watershed scale, terrestrial and aquatic agro-ecosystems throughout the world will be increasingly vulnerable to alterations in the precipitation and storage cycles.2 These changes, which are projected to continue, are already straining water resources and increasing irrigation demand.3
Notes
- 1.
Emmanuel Van Houtte and Johan Verbauwhede, “Operational Experience with Indirect Potable Reuse at the Flemish Coast,” Desalination 218, no. 1 (2008): 207.
- 2.
Petrus L. Du Pisani, “Direct Reclamation of Potable Water at Windhoek’s Goreangab Reclamation Plant,” Desalination 188, no. 1 (2006): 79–80.
- 3.
J. Lahnsteiner and G. Lempert, “Water Management in Windhoek, Namibia,” Water Science & Technology 55, no. 1 (2007): 446.
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© 2014 Hillary Brown
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Brown, H. (2014). Combating Water Stress and Scarcity: Augmented Sources and Improved Storage. In: Next Generation Infrastructure. Island Press, Washington, DC. https://doi.org/10.5822/978-1-61091-202-0_7
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DOI: https://doi.org/10.5822/978-1-61091-202-0_7
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