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Assessing water resources in China using PRECIS projections and a VIC model

机译:使用PRECIS预测和VIC模型评估中国的水资源

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摘要

Climate change is now a major environmental and developmentalissue, and one that will increase the challenge of sustainable waterresources management. In order to assess the implications of climate changefor water resources in China, we calibrated a Variable Infiltration Capacity(VIC) model with a resolution of 50×50 km2 using data from 125well-gauged catchments. Based on similarities in climate conditions, soiltexture and other variables, model parameters were transferred to otherareas not covered by the calibrated catchments. Taking runoff in the period1961–1990 as a baseline, we studied the impact of climate change on runoffunder three emissions scenarios, A2, B2 and A1B. Model findings indicatethat annual runoff over China as a whole will probably increase byapproximately 3–10% by 2050, but with quite uneven spatial and temporaldistribution. The prevailing pattern of "north dry and south wet" in Chinais likely to be exacerbated under global warming.
机译:现在,气候变化是一个重大的环境和发展问题,它将加剧可持续水资源管理的挑战。为了评估气候变化对中国水资源的影响,我们使用来自125个高位流域的数据对分辨率为50×50 km 2 的可变入渗能力(VIC)模型进行了校准。根据气候条件,土壤质地和其他变量的相似性,将模型参数转移到校准集水区未涵盖的其他区域。以1961-1990年的径流为基准,我们研究了在A2,B2和A1B这三种排放情景下气候变化对径流的影响。模型结果表明,到2050年,整个中国的年径流量可能会增加约3-10%,但时空分布相当不均匀。在全球变暖的情况下,中国普遍存在的“北干南湿”模式可能会加剧。

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