摘要
运用改进的综合气象干旱指数,根据洞庭湖流域19个气象站1961—2009年的实测气象资料,运用小波理论分析洞庭湖流域发生的干旱时间差异,并对洞庭湖流域的干旱特征进行空间格局分析。结果表明:从时间格局上,洞庭湖流域发生90%以上范围的干旱周期四季依次为:春季16a,夏季13 a,秋季9 a,冬季16 a;在空间格局上,洞庭湖流域干旱发生程度整体上是以衡阳、邵阳,芷江、通道以西,石门、南县以北三个地区为中心向其四周递减;从季节尺度来看,整体上秋季干旱最为严重,冬季次之,春季干旱最轻。
Based on the improved meteorological drought composite index and measured meteorological data from 19 meteorological stations in the watershed during the period from 1961 to 2009 , the time difference of the drought development in the watershed was analyzed through wavelet analysis , and the spatial pattern of the drought characteristics were analyzed .The results show that the primary cycles of drought that occurred in more than 90%of the coverage area in the watershed were 16 years in the spring , 13 years in the summer , nine years in the autumn , and 16 years in the winter; at the spatial scale , the most severe droughts occurred in the Hengyang-Shaoyang region , the western part of the Zhijiang-Tongdao region , and the northern part of the Shimen-Nanxian region , and the degree of drought decreased in the surrounding regions;and at the seasonal scale , the most severe droughts occurred in the autumn on the whole , followed by the winter , with the most slight droughts occurring in the spring .
出处
《河海大学学报(自然科学版)》
CAS
CSCD
北大核心
2014年第1期1-6,共6页
Journal of Hohai University(Natural Sciences)
基金
国家自然科学基金(41371052
U1203282)
水利部公益项目(201001066)
关键词
综合气象干旱指数
洞庭湖流域
干旱特征
时空格局
小波分析
meteorological drought composite index
Dongting Lake watershed
drought characteristics
spatial and temporal patterns
wavelet analysis