摘要
结合2000~2004年的资料,用SWAT模型构建了漳卫南流域分布式水文模型,对漳卫南流域的水量过程和水量平衡进行了模拟分析,并将模型模拟结果与海河流域水资源公报和实测水文站数据进行了比较。水平衡分析结果表明,流域内的来水项主要是降雨和灌溉水量,去水项主要是腾发量和汛期的径流量;该模型对于漳卫南流域水量模拟与实际比较一致。
With 2000~2004 basic data, Zhangweinan distributed hydrological model is build up based on SWAT model. The water quantity process and water balance of Zhangweinan is also simulated. The siumlated result is compared with the observed data of the hydrometric station and data from the Haihe Basin water resource bulletin. The simulated result of the water balance shows that the inlet water is mainly precipitation and irrigation, the water consumption is mainly evapotranspiration and runoff. The water quantity simulated result is accordant with the actual situation of the Zhangweinan Basin.
出处
《吉林大学学报(地球科学版)》
EI
CAS
CSCD
北大核心
2007年第5期949-954,共6页
Journal of Jilin University:Earth Science Edition
基金
国家自然科学基金项目(40401003)
世行GEF项目(HWCCZ5005)
关键词
SWAT
漳卫南流域
水量
水平衡
SWAT
Zhangweinan Basin
water quantity
water balance