自然资源学报 ›› 2013, Vol. 28 ›› Issue (11): 1988-1999.doi: 10.11849/zrzyxb.2013.11.015
林炳青1, 陈莹1,2, 陈兴伟1,2
收稿日期:
2012-08-03
修回日期:
2013-03-05
出版日期:
2013-11-20
发布日期:
2013-11-20
作者简介:
林炳青(1988-),男,福建漳州人,硕士研究生,主要从事水文学与水资源方面的研究。E-mail:bqlin2011@163.com
基金资助:
LIN Bing-qing1, CHEN Ying1,2, CHEN Xing-wei1,2
Received:
2012-08-03
Revised:
2013-03-05
Online:
2013-11-20
Published:
2013-11-20
Contact:
陈兴伟(1963-),教授,博士生导师。E-mail:cxwchen215@163.com
E-mail:cxwchen215@163.com
摘要: 探讨SWAT模型的敏感参数和参数值的区域差异,有助于减少水文过程模拟的不确定性,提高模型在不同区域的应用水平。论文在收集SWAT模型的国内应用文献基础上,依据干燥指数将流域划分为湿润区、半湿润区、半干旱区和干旱区,主要采用定性分析方法,分析模型的敏感参数和参数值的空间差异及其影响因素。结果表明,SWAT模型的敏感参数和参数值具有一定的区域差异。对于地表水文过程,径流曲线系数(CN2)和土壤可利用水量(SOL_AWC)在各个区域都比较敏感,土壤蒸发补偿系数(ESCO)在湿润区和半湿润区较为敏感;由于均受土壤质地的影响,湿润区CN2 值高于半湿润区,SOL_AWC则正好相反;受气温和植被覆盖的影响,湿润区和干旱区的ESCO取值高于半湿润区和半干旱区。地下水参数在湿润区和干旱区较为敏感。降雪融雪参数仅在干旱区融雪对径流贡献大的流域才比较敏感。由于气候、土壤、植被条件的区域异质性,导致了流域水文过程参数的区域差异。结果还表明,由于水文过程还受到局部气象条件、下垫面等多种因子共同作用,以及模型尚未揭示的其它因子的影响,模型参数在相同区域的不同流域也存在着一定的差异。
中图分类号:
林炳青, 陈莹, 陈兴伟. SWAT模型水文过程参数区域差异研究[J]. 自然资源学报, 2013, 28(11): 1988-1999.
LIN Bing-qing, CHEN Ying, CHEN Xing-wei. A Study on Regional Difference of Hydrological Parameters of SWAT Model[J]. JOURNAL OF NATURAL RESOURCES, 2013, 28(11): 1988-1999.
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