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A runoff map based on numerically simulated precipitation and a projection of future runoff in Iceland

机译:基于数值模拟降水的径流图和冰岛未来径流的预测

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The runoff of Iceland has been evaluated for the period 1961-1990, and changes in runoff from then to the period 2071-2100 predicted according to a future projection of climate change. The hydrological model WASIM-ETH was used, with meteorological data from the PSU/NCAR MM5 numerical weather model. The evaluation of the effects of climate change on water resources was based on a future climate simulation from the HIRHAM regional climate model with boundary conditions from the HadAM3H global climate model using A2 and B2 emissions scenarios. Future runoff was shown to become much higher in 2071-2100 compared to 1961-1990, predominantly due to increased glacial melt caused by increased temperature. Furthermore, changes in runoff seasonality would be substantial. Thus, according to this projection there could be great changes in hydropower production potential associated with climate change in Iceland.
机译:对冰岛的径流进行了1961-1990年的评估,并根据未来对气候变化的预测,预测了从那时到2071-2100年的径流变化。使用了水文模型WASIM-ETH,以及来自PSU / NCAR MM5数值天气模型的气象数据。对气候变化对水资源的影响的评估基于HIRHAM区域气候模型的未来气候模拟,以及使用A2和B2排放情景的HadAM3H全球气候模型的边界条件。与1961-1990年相比,2071-2100年的未来径流变得更高,这主要是由于温度升高导致冰川融化增加。此外,径流季节性的变化将是巨大的。因此,根据这一预测,与冰岛的气候变化有关的水电生产潜力可能会发生巨大变化。

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