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能量平衡融雪模型在西天山的应用试验
引用本文:庄毅璇,熊良时,徐俊荣,史志文. 能量平衡融雪模型在西天山的应用试验[J]. 安徽农业科学, 2011, 39(31): 19396-19398,19495
作者姓名:庄毅璇  熊良时  徐俊荣  史志文
作者单位:1. 重庆市环境保护工程设计研究院有限公司,重庆,400000
2. 中国科学院新疆生态与地理研究所,新疆乌鲁木齐,830011
3. 新疆交通科学研究院,新疆乌鲁木齐,830002
基金项目:中国科学院知识创新工程重要方向项目(KZCX2-YW-334)
摘    要:为了验证能量平衡融雪模型在巩乃斯流域的适用性,在天山积雪雪崩研究站开展了模型的应用试验。设置了3个融雪水收集样点,模拟值分别与1号、2号和3号样点观测的日融雪量进行对比,结果表明,1号融雪水收集点的拟合优度系数R2=0.86,体积差Dv=-5.9%;2号收集点R2=0.92,Dv=-3.2%;3号收集点,R2=0.91,Dv=-10.7%,模拟值总量偏高于实测值。较高的R2和较低的Dv值,表明模型达到了比较好的模拟效果,也显示该模型在巩乃斯河流域具有良好的应用前景。

关 键 词:融雪模型  能量平衡  净辐射  天山

Experiment on the Application of the Energy Balance Snowmelt Model on Western Tianshan Mountains
Affiliation:ZHUANG Yi-xuan et al(Chongqing Institute Corporation of Environmental Protecting and Design,Chongqing 400000)
Abstract:In order to verify the application of the energy balance snow melt model for the Gongnaisi River basin,an experiment of the model was performed in Tianshan Station of Snow Cover and Avalanche Research.There were three snow water collect sites in the experiment.By comparison between estimated snow water equivalent(SWE) and observed SWE of NO.1,NO2,NO.3 snow water collect sites,the results showed that two goodness of fit statistics for simulations,Nash-sutcliff coefficient(R2) and volume difference(Dv) were that R2=0.86,Dv=-5.9%(NO.1 snow water collect site);R2=0.92,Dv =-3.2% NO.2),R2=0.91,Dv=-10.7%(NO.3),respectively.The predictions had been overestimated somewhat.The high R2 and low Dv suggested that the model had good simulation effect and it can be applied in Gongnaisi River.
Keywords:Snowmelt model  Energy balance  Net radiation  Tianshan Mountains
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