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首页> 外文期刊>Agricultural and Forest Meteorology >Comparison of several surface resistance models for estimating crop evapotranspiration over the entire growing season in arid regions
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Comparison of several surface resistance models for estimating crop evapotranspiration over the entire growing season in arid regions

机译:比较几种估计干旱地区整个生长期作物蒸散量的表面阻力模型

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摘要

How to improve the reliability and accuracy of the single-layer Penman-Monteith (PM) model for estimating crop evapotranspiration (ET) over the entire growing season in arid regions, is still of great challenge for hydrologists. In the study, we developed a coupled surface resistance model (CO) after taking the combined restriction effect of vegetation and soil layers on ET into account. The CO model was compared with the modified Shuttleworth-Wallace model (MSW), and the traditional Jarvis, Katerji and Perrier, Irmak and Mutiibwa, Stannard, Leuning, Shuttleworth and Gurney, Massman, Garcia-Santos, Ortega-Farias, and Todorovic canopy resistance models over the partial and dense canopy stages. Maize and vineyard ET measured by the eddy covariance method during 2007-2013 were used to examine the model performance. Results indicate that the PM equation combined with the coupled surface resistance model yielded the lowest root mean square error against the other methods during all the years under either partial or dense canopy stages. Especially, the PM-CO method also performed superiorly against the dual-layer MSW model during the partial maize canopy period. After considering the meteorological, physiological and soil controls on surface resistance simultaneously, the coupled surface resistance model improved the accuracy significantly against the traditional canopy resistance models, and enhanced the reliability of the PM model for estimating partial canopy ET. Thus the coupled surface resistance equation integrated with PM model is recommended to estimate crop ET for the entire growth stages in arid regions. (C) 2015 Elsevier B.V. All rights reserved.
机译:对于水文学家来说,如何提高单层Penman-Monteith(PM)模型的可靠性和准确性,以估计整个生长季节的作物蒸散量(ET),仍然是一个巨大的挑战。在研究中,我们在考虑了植被和土壤层对ET的综合约束作用之后,开发了耦合表面电阻模型(CO)。将CO模型与改良的Shuttleworth-Wallace模型(MSW)以及传统的Jarvis,Kateji和Perrier,Irmak和Mutiibwa,Stannard,Leuning,Shuttleworth和Gurney,Massman,Garcia-Santos,Ortega-Farias和Todorovic冠层进行了比较局部和密集冠层阶段的阻力模型。通过涡度协方差方法在2007-2013年间测得的玉米和葡萄园ET用来检验模型性能。结果表明,在部分或密集冠层阶段,所有年份的PM方程与耦合表面电阻模型相结合均产生了最低的均方根误差。特别是,在部分玉米冠层期,PM-CO方法也比双层MSW模型表现更好。在同时考虑了气象,生理和土壤对表面阻力的控制之后,耦合表面阻力模型相对于传统的冠层阻力模型显着提高了精度,并增强了PM模型估算局部冠层ET的可靠性。因此,建议将耦合的表面电阻方程与PM模型集成在一起,以估计干旱地区整个生长阶段的作物ET。 (C)2015 Elsevier B.V.保留所有权利。

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