1. 陕西师范大学旅游与环境学院,陕西,西安,710062
2. 暨华中学,重庆,401120
3. 华阳中学,四川,成都,610213
纸质出版:2013
移动端阅览
彭维英, 殷淑燕, 朱永超, 等. 历史时期以来汉江上游洪涝灾害研究[J]. 水土保持通报, 2013,32(4):289-294.
PENG Wei-ying, YIN Shu-yan, ZHU Yong-chao, et al. Flood Disaster in Upper Reaches of Hanjiang River During Historical Period[J]. Bulletin of Soiland Water Conservation, 2013, 32(4): 289-294.
通过对汉江上游历史时期以来(208BC-2010AD)历史资料的搜集和整理
运用最小二乘法、小波分析和克里格插值等方法
对该区域洪涝灾害等级、时间(阶段、季节、周期等)和空间变化规律及成因进行了研究。结果表明
近2 220a间
汉江上游共发生洪涝灾害336次
平均6.6a发生1次
集中发生在夏秋季节(5-9月份)。该区域洪涝灾害划分为轻度洪灾、中度洪灾、重度洪灾和特大洪灾
分别占洪涝灾害总数的24.7%
29.5%
40.5%和5.3%。小波分析显示各级洪灾分别存在2~5a
38~40a
120a
160a的周期。洪涝灾害发生频率的变化呈现波动上升趋势
大致可分为3个阶段
清代道光年间前期、清代光绪年间和民国后期至20世纪末为洪涝灾害多发期。洪涝灾害空间分布差异明显
以安康盆地为中心向南、向北、向东、向西递减
存在两个高频中心和两个低频中心。大气环流异常
特殊地形条件
河流本身的水系特征
河道的弯曲程度及人类活动的影响是造成该区域洪涝灾害频发的主要原因。
The historical data about flood disaster was collected
reorganized and analyzed in upper reaches of Hanjiang River during the historical period(208BC-2010AD).By using least squares method
wavelet analysis
and the Kriging interpolation
the times when flood disaster occurred(stage
seasons
cycles
etc.)
the spatial variation and the causes of flood disaster were studied.The results showed that
during the past 2 220years
the flood disaster mainly occurred in the summer and Autumn(May to September)by 336times with a frequency of once every 6.6years in the upper reaches of Hanjiang River.The flood disaster could be divided into 4classes
mild
middle
great and serious floods
and each class accounted for 24.7%
29.5%
40.5% and 5.3%in the total numbers of floods
respectively.Wavelet analysis showed that
the period of each class was 2~5a
38~40a
120a
and 160a
respectively.The floods showed an increasing trend
and could be broadly divided into three stages.There were three flood-prone periods
the early Qing Dynasty of Emperor Daoguang's Reign
Qing Dynasty of Emperor Guangxu's Reign
and the Late Republic to the end of the 20th century.Flood disasters varied significantly at spatial scale
which were declined from Ankang Basin to periphery
and there are two high-frequency centers and two low-frequency centers.Atmospheric circulation anomalies
special terrain conditions
the river's water system characteristics
the degree of bending of the river and the impact of human activities are the main causes of flood disasters in this region.
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