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基于概率密度分析长江三角洲降水随时间的演变规律
引用本文:曾红玲,高新全,张文.基于概率密度分析长江三角洲降水随时间的演变规律[J].中国物理 B,2005,14(6):1265-1271.
作者姓名:曾红玲  高新全  张文
作者单位:State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;Key Laboratory of National Meteorological Bureau Climate Research Center, Beijing 100081, China;Key Laboratory of National Meteorological Bureau Climate Research Center, Beijing 100081, China; Department of Physics, Yangzhou University, Yangzhou 225009, China
基金项目:Project supported jointly by the National Key Program Development for Basic Research (Grant No. 2004CB418300) and the National Natural Sciences Foundation of China (Grant Nos. 40475027 and 40275031)
摘    要:将长江三角洲旱涝等级资料转换成降水概率随时间的演化,揭示了长江三角洲降水概率随时间演变的各层次的分布特征。结果表明:长江三角洲降水存在明显的年际、年代际以及世纪以上时间尺度的准周期变化,而且都超过0.05的信度检验。在530年旱涝等级序列中,虽然长江三角洲各地区发生旱、涝的小概率事件的频数不太相同,但由气候态背景(世纪尺度)所激发的小概率事件频数相同;这一研究结果充分说明作为背景状态的气候演变对小概率事件(干旱、洪涝)的发生具有非常重要的影响,对气候预测理论与提高气候预测准确率具有积极的指导作用。

关 键 词:旱涝  小概率事件  长江三角洲  概率演变
收稿时间:2004-11-23

Evolution characteristics of the precipitation in the Yangtze River delta based on the probability density
Zeng Hong-Ling,Gao Xin-Quan and Zhang Wen.Evolution characteristics of the precipitation in the Yangtze River delta based on the probability density[J].Chinese Physics B,2005,14(6):1265-1271.
Authors:Zeng Hong-Ling  Gao Xin-Quan and Zhang Wen
Abstract:The dryness/wetness (DW) grade data of the Yangtze River delta are transformed in this paper into the temporal evolution of precipitation probability (PP), and its hierarchically distributive characters are revealed. Research results show that the precipitation of the Yangtze River delta displays the interannual, interdecadal, as well as more than a century quasi-periodic changes, and the periods are all significant at a confidence level of more than 0.05. In the DW grade series of 530 years, although the frequency of the small probability events (SPEs) of drought/flood in each area of the Yangtze River delta is different, the frequency of the SPEs triggered by the climatic background state is yet the same. This research result fully narrates the significant impact of the climatic evolution as a background state upon the occurrence of SPEs, which will play an instructional role in climatic prediction theory and in raising the accuracy of climatic prediction.
Keywords:drought/flood  small probability events  Yangtze River delta  probability evolution
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