Spatially coherent climate projections are available– for example the 11 member ensemble produced by the UK Met Office [39] or the Future Flows datasets released by the Centre forEcology and Hydrology [73]. Given sufficient computing power and resources, it should be possible to use these datasets to repeat the national scale analysis of Duncan [5], but using a range of climate simulations in place of the baseline data. It is possible that a less detailed but more computationally tractable approach to this problem could also be found. If so, this would represent a valuable contribution to the hydropower literature.
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