基于新安江模型的曲江流域水文模拟研究
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摘要
水文模型在水文理论研究和实践中具有重要意义。将曲江流域西山水文站以上区域作为研究对象,分析了新安江模型在该区域的适用情况。结果表明:新安江模型在曲江流域模拟效果良好,Nash效率系数多在0.7以上,水量平衡误差也基本控制在±10%以内;资料序列的长度对模拟效果影响显著,长序列资料的峨山站和西山站模拟结果明显优于短序列的大矣资站和马家庄站;新安江模型能较好适用于我国南方山区,对研究变化环境下水文过程的响应具有良好的适用性。
Hydrological model plays an important role in hydrological theory research and practice.Taking the above area of Xishan hydrological station in Qujiang River basin as a study area,the applicability of the Xin'Anjiang model in this area was analyzed.The results show that Xin'anjiang model performs well in the simulation in Qujiang River basin,with Nash coefficient above 0.7 and the error of water balance controlled within ± 10% for most catchments.The length of data sequence has significant influence on simulation effect.The simulation results in the stations with longer length of data sequence like Eshan and Xishanare are much better than in Dayizi and Majiazhuang stations.The Xin'anjiang model is suitable for the mountainous areas of southern China,and has good applicability to the study of the hydrological process in the changing environment.
Hydrological model plays an important role in hydrological theory research and practice.Taking the above area of Xishan hydrological station in Qujiang River basin as a study area,the applicability of the Xin'Anjiang model in this area was analyzed.The results show that Xin'anjiang model performs well in the simulation in Qujiang River basin,with Nash coefficient above 0.7 and the error of water balance controlled within ± 10% for most catchments.The length of data sequence has significant influence on simulation effect.The simulation results in the stations with longer length of data sequence like Eshan and Xishanare are much better than in Dayizi and Majiazhuang stations.The Xin'anjiang model is suitable for the mountainous areas of southern China,and has good applicability to the study of the hydrological process in the changing environment.
引文
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[14]徐莎,杨小柳.GR3模型和新安江模型在我国的对比研究[J].水文,2015,35(1):7-13.
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[19]杨自坤,孔燕.新安江三水源模型在横江洪水预报中的应用[J].水资源研究,2010,31(1):36-38.
[2]KHAN M H.Xinanjiang Model on Bird Creek catchment in USA.[J].Pakistan Journal of Agricultural Research,1993,14(4):373-382.
[3]ZHU Dehua,PENG Dingzhi.Notice of Retraction Comparison of the hydrological models in the Upper Medway Catchment,UK[C]//Sixth International Conference on Natural Computation.IEEE,2010:3874-3877.
[4]刘玉龙,阮本清,张春玲,等.从生态补偿到流域生态共建共享——兼以新安江流域为例的机制探讨[J].中国水利,2006(10):4-8.
[5]HAPUARACHCHI H A P,LI Zhijia,WANG Shouhui.Application of SCE-UA method for calibrating the Xinanjiang watershed model[J].湖泊科学(英文版),2001,13(4):304-314.
[6]刘金涛,宋慧卿,张行南,等.新安江模型理论研究的进展与探讨[J].水文,2014,34(1):1-6.
[7]张波,马得莲,包为民,等.新安江模型在富水水库流域洪水预报中的应用[J].水电能源科学,2010,28(4):49-51+21.
[8]胡宇丰,安波,陆玉忠,等.新安江模型在嫩江流域洪水预报中应用[J].东北水利水电,2011,29(8):41-45+72.
[9]肖兴涛,张鹏远,张淑霞.新安江模型在汤旺河流域洪水预报中的应用[J].黑龙江水利科技,2012,40(1):41-43.
[10]张漫莉.改进的HBV模型与新安江模型在武江流域洪水预报中的应用比较[J].人民珠江,2014,35(1):34-37.
[11]周广刚,温立成,侯国柱.三水源新安江模型在洒河流域的适用性研究[J].水利水电工程设计,1999(3):45-47.
[12]朱求安,张万昌.新安江模型在汉江江口流域的应用及适应性分析[J].水资源与水工程学报,2004,15(3):19-23.
[13]唐俊龙,郝振纯.新安江模型在浙江白水坑水库的适用性研究[J].水电能源科学,2017,35(3):20-23.
[14]徐莎,杨小柳.GR3模型和新安江模型在我国的对比研究[J].水文,2015,35(1):7-13.
[15]谷桂华.玉溪市暴雨洪水特性分析[C]//中国水利学会2003学术年会,深圳:2003.
[16]孙惠玲,李天艳,周晓娟,等.近54年来玉溪市气候变化特征分析[J].云南师范大学学报(自然科学版),2016,36(5):67-73.
[17]张利茹,管仪庆,叶彬,等.新安江模型参数敏感性分析的实证研究[J].水电能源科学,2008,26(5):16-17+30.
[18]舒畅,刘苏峡,莫兴国,等.新安江模型参数的不确定性分析[J].地理研究,2008,27(2):343-352.
[19]杨自坤,孔燕.新安江三水源模型在横江洪水预报中的应用[J].水资源研究,2010,31(1):36-38.