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Long-term trend of major climate variables in the Taihu basin during the last 53 years

机译:过去53年中太湖流域主要气候变量的长期趋势

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Recently, frequent occurrence of extreme flood events associated with the hydrological cycle accelerated by climate change in the Taihu basin have received significant attention by both local and central governments in China. Detection of the plausible long-term trend for climate variables is the first step to understand the effects of climate change on floods. On the basis of monthly time series of precipitation, mean air temperature, relative humidity and sunshine duration in the Taihu basin from 1954 to 2006, the spatio-temporal patterns of long-term trend for these climate variables during the past 53 years were detected and analysed by using the nonparametric Mann-Kendall test and departure curve method. The results showed that the mean air temperature increased by 1.43° in the Taihu basin during the past 53 years, and the annual mean precipitation increased by 10.44 mm with more temporal and spatial variability, while the annual mean relative humidity and annual sunshine duration exhibited a decreasing tendency, with 10-year decreasing rates of -0.99% and -7.797 h, respectively. In addition, the Hurst index was adopted to detect the long-range dependence for the time series of these climate variables, which showed that the annual mean precipitation in the Taihu basin would continue to increase in the future, similar to the trend of mean air temperature, whilst the annual mean relative humidity and annual sunshine duration would continue to decrease, being consistent with that for the last 53 years. The results of this study could be used to provide technical support for flood control and drought relief in urban planning and construction under future global climate change in the Taihu basin.
机译:近年来,太湖流域与气候变化加速的水文循环有关的极端洪水事件频繁发生,已引起中国地方和中央政府的高度重视。了解气候变量可能的长期趋势是了解气候变化对洪水的影响的第一步。根据1954年至2006年太湖流域的每月降水,平均气温,相对湿度和日照时数的时间序列,发现了过去53年中这些气候变量的长期趋势的时空格局,并使用非参数Mann-Kendall检验和偏离曲线法进行分析。结果表明,太湖流域近53年平均气温升高1.43°,年均降水量增加10.44mm,时空变化较大,年平均相对湿度和日照时间呈上升趋势。下降趋势,十年下降率分别为-0.99%和-7.797 h。此外,采用赫斯特指数来检测这些气候变量的时间序列的长期相关性,这表明未来太湖流域的年平均降水量将继续增加,类似于平均空气的趋势。温度,而年平均相对湿度和日照时间将持续减少,与过去53年的温度一致。研究结果可为太湖流域未来全球气候变化下城市规划建设中的防洪抗旱提供技术支持。

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