水资源与水工程学报2012，Vol.23Issue(3)：51-54,57,5.
阿克苏河源流径流模拟初探
Simulation of runoff process in headstream of Aksu River
摘要
Abstract
It is difficult to make research on hydrology system in alpine mountains due to bad natural conditions, rare ground observing stations and limit availability of observing condition. The special natural and geographical conditions not only make the processes of studying hydrology much complicated, but also hinder the development of exploring the processes and principles of hydrology system in the alpine cold areas. Snowmelt structure of Xinanjiang model was applied to simulate runoff process of Kumalike River, a part of Aksu River, and validated according to the statistical data of runoff collected from hydrology stations. The results demonstrated that Xinanjiang model could be used to simulate the runoff process in alpine cold regions under the condition lack of hydrological and weather data, and it has a better consistency with the actual situation, the relative error of runoff volume is less than 15% , however, the simulating precision need to be improved. The thesis could provide good reference for the further study of runoff processes in the alpine cold areas.关键词
融雪结构/新安江模型/高寒山区/库玛力克河流域Key words
snowmelt structure/ Xinanjiang model/ alpine mountains/ Kumalikehe River分类
天文与地球科学引用本文复制引用
王鹏,姜卉芳,穆振侠..阿克苏河源流径流模拟初探[J].水资源与水工程学报,2012,23(3):51-54,57,5.基金项目
水利部公益项目(201001065) （201001065）
新疆水文学及水资源重点学科基金资助(xjsxszydxk20101202) （xjsxszydxk20101202）
新疆农业大学校前期课题资助(XJAU201005) （XJAU201005）
