长江流域资源与环境 >> 2014, Vol. 23 >> Issue (03): 434-.doi: 10.11870/cjlyzyyhj201403019

• 鄱阳湖研究 • 上一篇    下一篇

近50年来鄱阳湖流域降雨多时间尺度变化规律研究

原立峰|杨桂山| |李恒鹏, 张增信   

  1. (1.南京邮电大学地理与生物信息学院,江苏 南京210003|2.中国科学院南京地理与湖泊研究所,江苏 南京210008|3.虚拟地理环境教育部重点实验室,江苏 南京210046;4.南京林业大学江苏省林业生态工程重点实验室,江苏 南京210037
  • 出版日期:2014-03-20

RAINFALL MULTIPLE TIME SCALE VARIATION RULE OF POYANG LAKE BASIN IN THE PAST 50 YEARS

YUAN Lifeng1, 2, 3|YANG Guishan2| LI Hengpeng2| ZHANG Zengxin4   

  1. (1.College of Geography &|Biological Information, Nanjing University of Posts and Telecommunications, Nanjing 210003,China|2.Nanjing Institute of Geography and Limnology,Chinese Academy of Science, Nanjing 210008,China; 3.Key Laboratory of Virtual Geographic Environment, Ministry of Education, Nanjing 210046,China|4.Jiangsu Key Laboratory of Forestry Ecological Engineering, Nanjing Forestry University, Nanjing 210037,China
  • Online:2014-03-20

摘要:

利用鄱阳湖流域16个气象站1960~2008年共49 a的月降雨资料,采用Morlet小波函数,对该流域降雨季节变化、年际和年代际时间序列进行小波分析,揭示了流域降雨变化的多时间尺度特征,分析了不同时间尺度下降雨序列变化的周期和突变点。研究表明:①1960~1990年,年降雨量呈明显年际和代际振荡,并无显著趋势;进入90年代以后,年降雨呈现显著上升趋势;进入21世纪,尤其从2002年开始,年降雨量开始减少;②流域季节降雨和年降雨都存在多时间尺度特征,夏季降雨、冬季降雨和年降雨都存在18 a的第一主周期;春季、冬季和年降雨存在6 a次主周期;此外,春季、秋季、冬季和年降雨均存在3 a次主周期;③夏季降雨在18 a时间尺度上与年降雨变化具有相同的趋势和相位,春季降雨在3 a和6 a时间尺度上与年降雨变化具有相似趋势和相位变化

Abstract:

A total of 49 years of monthly rainfall data in 16 meteorological stations in Poyang Lake basin during 1960 to 2008 was analyzed by Morlet wavelet function.The rainfall seasonal, interannual and interdecadal time series analysis results were used to reveal the multiple time scale features of rainfall change, 〖JP+1〗and the periodic variation and mutation points of rainfall sequences at different time scales.(1) Annual rainfall showed obvious interannual and decadal oscillations during 1960 to 1990, no significant trend, but the annual rainfall had a significant increasing trend after entering the 1990s.The annual rainfall was decreasing from 2002.〖JP〗In general, spring rainfall had a decreasing trend during the study period and a decreasing amplitude of -1103 mm/10 a; summer rainfall had an increasing trend and an increasing amplitude of 2512 mm/10 a; autumn rainfall had a decreasing trend and a decreasing amplitude of -416 mm/10 a; winter rainfall had an increasing trend and an increasing amplitude of 11.85mm/10a.Annual rainfall had an increasing trend in Poyang Lake Basin and an increasing amplitude of 2179 mm/10 a.(2) Both seasonal and annual rainfall had multiple time scale features, and there was 18 a first principal period in summer, winter and annual rainfall.Annual rainfall experienced three circulations from few to more on 18 a time scales, and the mutational point happened in the year of 1970, 1980, 1992 and 2003.At present, annual rainfall is in the less period.There is 6 a second principal period in spring, winter and annual rainfall.In additional, there is 3 a third principle period in spring, autumn, winter and annual rainfall.(3) Summer and annual rainfall had the same trend and phase changes in the 18 a time scale,while the spring and annual rainfall had similar trend and phase changes in 3 a and 6 a time scales.In 6 a time scale, change rule of spring rainfall and annual rainfall was more similar than that of summer rainfall and annual rainfall.The corresponding relationship was different between changing pattern of spring and annual rainfall and that of summer and annual rainfall in different time scales, and smaller was the time scale, smaller was the phase difference.(4) The seasonal changes trend in the study period was followed the order of Spring>summer>autumn>winter in the 1960s, 1970, 1980 and 2000s.Annual rainfall in the 1990s was obviously more than other periods, which was caused by that summer rainfall was greater than spring rainfall and winter rainfall was greater than autumn rainfall

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