The water impacts of climate change mitigation measures
Philip Wallis (),
Michael Ward,
Jamie Pittock,
Karen Hussey,
Howard Bamsey,
Amandine Denis,
Steven Kenway,
Carey King,
Shahbaz Mushtaq,
Monique Retamal and
Brian Spies
Climatic Change, 2014, vol. 125, issue 2, 209-220
Abstract:
A variety of proposed activities to mitigate greenhouse gas emissions will impact on scarce water resources, which are coming under increasing pressure in many countries due to population growth and shifting weather patterns. However, the integrated analysis of water and carbon impacts has been given limited attention in greenhouse mitigation planning. In this Australian case study, we analyse a suite of 74 mitigation measures ranked as highest priority by one influential analysis, and we find that they have highly variable consequences for water quantity. We find: (1) The largest impacts result from land-based sequestration, which has the potential to intercept large quantities of water and reduce catchment yields, estimated to exceed 100 Mm 3 /MtCO 2 -e of carbon mitigated (100,000 l per tonne CO 2 -e). (2) Moderate impacts result from some renewable power options, including solar thermal power with a water cost estimated at nearly 4 Mm 3 /MtCO 2 -e. However, the water impacts of solar thermal power facilities could be reduced by designing them to use existing power-related water supplies or to use air or salt-water cooling. (3) Wind power, biogas, solar photovoltaics, energy efficiency and operational improvements to existing power sources can reduce water demand through offsetting the water used to cool thermal power generation, with minor savings estimated at 2 Mm 3 /MtCO 2 -e and amounting to nearly 100 Mm 3 of water saved in Australia per annum in 2020. This integrated analysis significantly changes the attractiveness of some mitigation options, compared to the case where water impacts are not considered. Copyright Springer Science+Business Media Dordrecht 2014
Date: 2014
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Persistent link: https://EconPapers.repec.org/RePEc:spr:climat:v:125:y:2014:i:2:p:209-220
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DOI: 10.1007/s10584-014-1156-6
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