Arid
半干旱沙地-草甸区水面蒸发模拟及其影响因子辨识
其他题名Simulating evaporation from a water surface for the sand-meadow ecotone of the semiarid region in North China
童新1; 刘廷玺1; 杨大文2; 段利民1; 吴尧1; 王天帅1; 王海燕1; 高肖彦1
来源期刊干旱区地理
ISSN1000-6060
出版年2015
卷号38期号:1页码:10-17
中文摘要在分析半干旱沙地一草甸区的水面蒸发过程及其影响因子的基础上,釆用多元逐步回归分析方法,对水面蒸发的众多影响因子进行逐步筛选,找出显著影响因子,建立水面蒸发与其显著影响因子间的多元非线性回归模型,并模拟计算了彭曼蒸发公式、道尔顿水汽运输理论蒸发公式中的风函数,比较分析了彭曼模型、变异道尔顿模型、多元非线性回归模型计算的水面蒸发量。结果表明:彭曼模型、变异道尔顿模型和最终建立的多元非线性逐步回归模型所得结果十分接近,与实测水面蒸发量的趋势也很一致;除变异道尔顿模型稳定性稍差外,其余两者都具有较好的稳定性;多元非线性逐步回归方法可以找到水面蒸发的显著影响因子,剔除掉不显著影响因子,避免因子相关造成的影响,使所建回归模型具有良好的拟合效果,其决定系数达到了0.773,预测结果令人满意。
英文摘要The southern Horqin sandy land,about 70 km away from Tongliao City,Inner Mongolia,China,is a typical sandy land in North China with limited water resources and fragile ecosystems. Quantification of evaporation from water surfaces over this region is critical to developing an understanding of eco-hydrological processes and therefore could be helpful to ecological restoration and water resources management over the arid region. In this study,processes and factors of water surface evaporation in the sand-oasis ecotone of the semiarid region were analyzed using data collected at the Agula Eco-hydrological Experimental Station. Then the stepwise multivariate regression analysis was applied to identify meteorological factors that primarily determine water surface evaporation. Furthermore, multivariate nonlinear stepwise regression forecasting models between water surface evaporation and the selected factors were built. Both the Dalton equation and Penman equation were used in this study to compute evaporation from water surfaces,with their wind functions being modified based on the observed wind velocity at 2 m height above the water surface. Finally the multivariate nonlinear stepwise regression models were compared with evaporation estimated from the Penman equation and Dalton equation. By using the multivariate stepwise regression analysis method,factors with varying significance could be ordered,with insignificant factors being removed from the subsequent analysis and factor correlation being reduced. Wind speed,saturated vapor pressure deficit and net radiation were identified as three most important factors determining water surface evaporation in the study area. The fitting of the optimal equation was satisfactory,indicating a coefficient of determination of 0.77 between the original equation and the optimized equation. All these forecasting models were generally consistent with the observations. Results of daily evaporation from the Dalton equation,the Penman equation and the optimal equation were almost the same, with a root mean square error of 1.98 mm, 2.21 mm and 1.87 mm between the modeled evaporation and observed evaporation during the calibration period,and 2.63 mm,3.22 mm and 2.93 mm during the validation period for these three equations,respectively. Both the Dalton equation and the Penman equation whose parameters of the wind function were optimized to accommodate characteristics of the study region could perform well in simulating water surface evaporation.
中文关键词多元非线性逐步回归分析 ; 彭曼模型 ; 变异道尔顿模型 ; 水面蒸发 ; 显著影响因子
英文关键词multivariate nonlinear stepwise regression analysis Penman model variation of Dalton model water surface evaporation significant factor
语种中文
国家中国
收录类别CSCD
WOS类目GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向Geology
CSCD记录号CSCD:5349247
来源机构内蒙古农业大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/232634
作者单位1.内蒙古农业大学水利与土木建筑工程学院, 呼和浩特, 内蒙古 010018, 中国;
2.清华大学水利水电工程系, 水沙科学与水电工程国家重点实验室, 北京 100084, 中国
推荐引用方式
GB/T 7714
童新,刘廷玺,杨大文,等. 半干旱沙地-草甸区水面蒸发模拟及其影响因子辨识[J]. 内蒙古农业大学,2015,38(1):10-17.
APA 童新.,刘廷玺.,杨大文.,段利民.,吴尧.,...&高肖彦.(2015).半干旱沙地-草甸区水面蒸发模拟及其影响因子辨识.干旱区地理,38(1),10-17.
MLA 童新,et al."半干旱沙地-草甸区水面蒸发模拟及其影响因子辨识".干旱区地理 38.1(2015):10-17.
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