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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Statistical behaviours of precipitation regimes China and their links with atmospheric circulation 1960-2005
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Statistical behaviours of precipitation regimes China and their links with atmospheric circulation 1960-2005

机译:1960-2005年中国降水状况的统计行为及其与大气环流的联系

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this study, we comprehensively analysed daily precipitation time series of 590 rastations China covering 1960-2005. Ten indices were defined to evaluate changing patterns of precipitation regimes and trend detection was performed using Mann-Kendall trend test and linear regressive technique. For the sake of better understanding of underlying causes behind changing properties of precipitation regimes, we also investigated spatial and temporal variations of atmospheric circulation of water vapour flux. The results revealed different changing properties of precipitation events across China. Generally, wet tendency was identified the south China and dry tendency north China. Besides, slight wet tendency could be found northwest China. addition, increasing precipitation intensity could be observed mainly the lower Yangtze River basand the Pearl River basin. Remarkable seasonal shifts of wet/dry conditions were also detected China: wet tendency winter and dry tendency summer. Furthermore, this study revealed good agreement between spatial distribution of precipitation regimes and water vapour flux, showing tremendous influences of water vapour flux on the precipitation changes across China. Regions east to 100°E were dominated by increasing water vapour flux winter. Weaker East Asian Summer Monsoon was the macause responsible for decreasing northward propagation of water vapour flux, causing different wet (dry) tendency south (north) China. This study can provide theoretical evidence for effective water resource management and sound arrangement of agriculture activities on river basscale under the changing environment across China.
机译:这项研究,我们全面分析了1960-2005年中国590个暴动的日降水时间序列。定义了十个指数以评估降水状况的变化模式,并使用Mann-Kendall趋势检验和线性回归技术进行了趋势检测。为了更好地了解降水机制变化背后的根本原因,我们还研究了大气水汽通量循环的时空变化。结果揭示了中国降水事件的不同变化特征。通常,华南地区确定为湿润趋势,华北地区确定为干燥趋势。此外,在中国西北地区可能会出现轻微的湿润趋势。此外,降水强度的增加主要集中在长江下游和珠江流域。在中国,也发现了干湿状况的明显季节性变化:中国的冬季湿润趋势和夏季的干燥趋势。此外,这项研究揭示了降水制度的空间分布与水汽通量之间的良好一致性,显示了水汽通量对中国降水变化的巨大影响。东经100°E的地区主要是冬季水汽通量增加。东亚夏季风减弱,是导致水汽通量向北传播减少的原因,导致中国南方(北部)出现不同的湿(干)趋势。这项研究可以为中国不断变化的环境下有效的水资源管理和巴斯河规模农业活动的合理安排提供理论依据。

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