Sanjiang Plain,located in the northeast of Heilongjiang Province,is one of the important grain producing areas in Heilongjiang Province,which has made great contributions to China's grain industry.However,the rapi...Sanjiang Plain,located in the northeast of Heilongjiang Province,is one of the important grain producing areas in Heilongjiang Province,which has made great contributions to China's grain industry.However,the rapid development of agriculture has increased the demand for water resources,and the water cycle process has been damaged,which has caused a series of problems,and the adverse effects have aroused great concern from all sides.In order to study the evolution law of precipitation and runoff in the lower Songhua River basin of Sanjiang Plain,the monthly precipitation data of Fujin,Jiamusi and Yilan meteorological stations and the measured runoff data of Jiamusi and Changjiangtun hydrological stations of the Songhua River from 1956 to 2011 were used.Mann-Kendall method,Hurst index method,sliding T test and wavelet analysis were used to analyze the trend,mutability and periodicity of precipitation and runoff evolution.The results show that the annual precipitation and runoff of the lower Songhua River basin in Sanjiang Plain showed a downward trend in the past 56 years(1956-2011);the mutation time of precipitation at Fujin Station,Jiamusi Station and Yilan Station was 1987,1959 and 2007,1973,respectively,the mutation time of runoff at Jiamusi Station and Changjiangtun Station appeared in 1967 and 1988;the first main periods of the annual precipitation wavelets are 42 years,54 years and56 years,respectively,and the periods are about 28-31 years,36-39 years and 36-38 years,the annual runoff of Jiamusi Station has the first main period of 57 years and the period is about 37-40 years,and the annual runoff of Changjiangtun Station has the first main period of 35 years and the period is about 20-24 years;the freeze-thaw process has significant influence on runoff in the study area.The results of this study have practical significance for rational planning and utilization of surface water resources and joint operation of surface water and groundwater in Sanjiang Plain.展开更多
基金funded by Northeast Institute of Geography and Agroecology,Chinese Academy of Sciences commissioned the project Research and Application of Key Technologies of Water Resources Allocation in Ten Million mu Irrigated Area of Sanjiang Plain,grant number XDA28100105。
文摘Sanjiang Plain,located in the northeast of Heilongjiang Province,is one of the important grain producing areas in Heilongjiang Province,which has made great contributions to China's grain industry.However,the rapid development of agriculture has increased the demand for water resources,and the water cycle process has been damaged,which has caused a series of problems,and the adverse effects have aroused great concern from all sides.In order to study the evolution law of precipitation and runoff in the lower Songhua River basin of Sanjiang Plain,the monthly precipitation data of Fujin,Jiamusi and Yilan meteorological stations and the measured runoff data of Jiamusi and Changjiangtun hydrological stations of the Songhua River from 1956 to 2011 were used.Mann-Kendall method,Hurst index method,sliding T test and wavelet analysis were used to analyze the trend,mutability and periodicity of precipitation and runoff evolution.The results show that the annual precipitation and runoff of the lower Songhua River basin in Sanjiang Plain showed a downward trend in the past 56 years(1956-2011);the mutation time of precipitation at Fujin Station,Jiamusi Station and Yilan Station was 1987,1959 and 2007,1973,respectively,the mutation time of runoff at Jiamusi Station and Changjiangtun Station appeared in 1967 and 1988;the first main periods of the annual precipitation wavelets are 42 years,54 years and56 years,respectively,and the periods are about 28-31 years,36-39 years and 36-38 years,the annual runoff of Jiamusi Station has the first main period of 57 years and the period is about 37-40 years,and the annual runoff of Changjiangtun Station has the first main period of 35 years and the period is about 20-24 years;the freeze-thaw process has significant influence on runoff in the study area.The results of this study have practical significance for rational planning and utilization of surface water resources and joint operation of surface water and groundwater in Sanjiang Plain.
