喀尔勒克河洪水成因分析及洪水计算  

Flood Cause Analysis and Flood Calculation of the Karlek River

作　　者：皇甫科威 HUANGFU Ke-wei

机构地区：[1]塔城水利设计研究院有限公司,新疆塔城834700

出　　处：《山西水利科技》2024年第2期59-62,共4页Shanxi Hydrotechnics

摘　　要：喀尔勒克河发源于萨吾尔山南坡,河流长150 km,流域面积1633 km^(2),流域属于寒湿带大陆性干旱气候,降水较少。以喀尔勒克河为研究对象,分析了洪水成因,以哈拉依敏站、马拉苏站、乌什水站、白杨河730站为参证站,采用了地区综合法计算了该河流的设计洪水,以期为新疆地区河流洪水成因分析和设计洪水计算提供理论借鉴。The Karlek River originates from the southern slope of Sawuer Mountain.It is 150 km long and covers an area of 1633 km^(2).The river basin belongs to the cold and humid continental arid climate with less precipitation.Taking Karlek River as the research object,the flood causes were analyzed first,and then the design flood of the river was calculated by using the regional comprehensive method with Halayimin Station,Malasu Station,Wushishui Station and Baiyanghe No.730 Station as reference stations.The results could provide theoretical reference for the analysis of river flood causes and design flood calculation in Xinjiang region.

关 键 词：喀尔勒克河 洪水成因 设计洪水 

分 类 号：TV122[水利工程—水文学及水资源]