Estimation of Evapotranspiration Based on a Modified Penman-Monteith-Leuning Model Using Surface and Root Zone Soil Moisture

被引:6
作者
Duan, Hao [1 ,2 ]
Zhao, Hongli [1 ,2 ]
Li, Qiuju [2 ,3 ]
Xu, Haowei [1 ,2 ]
Han, Chengxin [1 ,2 ,4 ]
机构
[1] China Inst Water Resources & Hydropower Res, Dept Water Resources, Beijing 100048, Peoples R China
[2] Minist Water Resources, Key Lab River Basin Digital Twinning, Beijing 100083, Peoples R China
[3] China Univ Geosci, Sch Water Resources & Environm, Beijing 100083, Peoples R China
[4] Lanzhou Jiaotong Univ, Fac Geomatics, Lanzhou 730070, Peoples R China
基金
中国国家自然科学基金;
关键词
evapotranspiration; Penman-Monteith; soil moisture; ERA5; GLDAS; EVAPORATION; UNCERTAINTY; ENERGY;
D O I
10.3390/w15071418
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Most of the current parameterization schemes for the Penman-Monteith-Leuning evapotranspiration (ET) model (PML) consider meteorological and energy factors and land use types, but the analysis of the effect of soil moisture (SM) changes on ET processes lacks sufficient attention. This paper proposes a parameterization scheme for the sensitive parameters of the PML model considering soil water content, i.e., coupling the land surface SM in the calculation of soil evaporation coefficient f and coupling the SM of the root zone layer in the calculation of maximum stomatal conductance g(sx), respectively. The new parameterization scheme is validated at 13 flux sites worldwide and showed significant improvements in improving the correlation with measured values. Moreover, based on the analysis of the spatial distribution of soil evaporation and vegetation transpiration, and the correlation between SM and ET, the regional characteristics of the effect of SM on ET are further revealed. This study provides a new idea for conducting the fusion simulation of SM based on a PML model, which is useful for the subsequent development of the model.
引用
收藏
页数:15
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