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黔西南地区旱涝态势变化规律分析
引用本文:师鹏飞,杨涛,张和喜,杨静.黔西南地区旱涝态势变化规律分析[J].水电能源科学,2014,32(11):1-4.
作者姓名:师鹏飞  杨涛  张和喜  杨静
作者单位:河海大学 水文水资源与水利工程科学国家重点实验室, 江苏 南京 210098;河海大学 水文水资源与水利工程科学国家重点实验室, 江苏 南京 210098;贵州省水利科学研究院, 贵州 贵阳 550000;贵州省水利科学研究院, 贵州 贵阳 550000
基金项目:水利部公益性行业科研专项经费项目(201201025);国家自然科学基金面上项目(41371051);江苏省普通高校研究生科研创新计划项目(CXLX13_240)
摘    要:为探明黔西南地区旱涝态势的变化规律,以黔西南地区望谟县为例,基于标准化降水指数,结合概率统计、趋势拟合、小波分析等方法分析了望谟县1959~2013年的旱涝强度、频率、年代际变化、季节性变化以及周期性变化。结果表明,望谟县发生极端旱涝事件的概率较大,1960s~2010s时间序列内均有水文极端事件发生,尤其是2000年以后,旱涝极端事件的振幅较以往呈现增大趋势,未来几年望谟县可能还会遭受极端干旱事件;旱涝态势年代际变化存在3个主要变化阶段,即1960s~1970s旱涝态势明显转变,1970年以后保持规律的旱涝交替,2000年以后呈现旱涝不平衡的状态,干旱态势占主导;春季和秋季呈现向干旱发展的趋势,夏季和冬季无明显变化;标准化降水指数存在以21~22年为主周期的变化规律。

关 键 词:多尺度    极值    旱涝态势    时间变化    周期    望谟县

Change Law of Drought and Flood Situation in Qianxinan Area
SHI Pengfei,ANG Tao,ZHANG Hexi and YANG Jing.Change Law of Drought and Flood Situation in Qianxinan Area[J].International Journal Hydroelectric Energy,2014,32(11):1-4.
Authors:SHI Pengfei  ANG Tao  ZHANG Hexi and YANG Jing
Affiliation:State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China;State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China;Guizhou Hydraulic Research Institute, Guiyang 550000, China;Guizhou Hydraulic Research Institute, Guiyang 550000, China
Abstract:Wangmo county is selected as a typical area in Qianxinan state to investigate the temporal patterns of drought and flood during the period of 1959-2013. Temporal patterns including intensity, frequency, inter-annual and seasonal variability, and periodic feature of drought and flood in Wangmo county are investigated by using the standardized precipitation index (SPI) incorporating with probabilistic method, trend analysis and wavelet analysis method. The results indicate that there exists a large probability of appearance of extreme drought and flood; extreme events seem to be occurring frequently from 1960s to 2010s, and the intensity of extremes after 2000 seem to be greater than before; Wangmo county will probably suffer extreme drought in the nearly coming years to a great extent; the inter-annual variability show characteristics of phases: drought and flood events appear a great transformation in the period 1960s-1970s; keeping regular alternate until unbalanced drought and flood appeared after 2000, during which drought dominates; spring and autumn tend to be drought, while summer and winter keep stable; the SPI changes with a primary period of 21-22 a.
Keywords:multiple scales  extreme value  drought and flood situation  temporal patterns  periodicity  Wangmo county
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