A nonlinear function approach for the normalized complementary relationship evaporation model

被引:69
|
作者
Han, Songjun [1 ,2 ,3 ]
Hu, Heping [1 ]
Tian, Fuqiang [1 ]
机构
[1] Tsinghua Univ, Dept Hydraul Engn, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[2] China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100048, Peoples R China
[3] Natl Ctr Efficient Irrigat Engn & Technol Res, Beijing 100048, Peoples R China
基金
中国国家自然科学基金;
关键词
evaporation; potential evaporation; complementary relationship; normalization; advection-aridity model; ADVECTION-ARIDITY APPROACH; REGIONAL EVAPOTRANSPIRATION; DESERT; WATER;
D O I
10.1002/hyp.8414
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
A nonlinear function approach for the normalized complementary relationship evaporation model that is different from the methodology maintaining the symmetric complementary relationship with appropriate definitions of potential and wet-environment evaporation is proposed and verified. This approach employs the definitions used in the advection-aridity model, wherein the potential is estimated using the Penman equation. Normalized by Penman potential evaporation, the complementary relationship model is expressed as a function describing the relationship between the evaporation ratio (the ratio of the actual to the Penman potential evaporation) and the proportion of the radiation term in Penman potential evaporation. The new nonlinear function proposed in the current study is approximately equivalent to the advection-aridity and the modified Granger models under conditions that are neither too wet nor too dry, but is more reasonable under arid and wet conditions. The new nonlinear function model performs well in estimating actual evaporation, as verified by the observed data from four sites under different land covers. Copyright (c) 2011 John Wiley & Sons, Ltd.
引用
收藏
页码:3973 / 3981
页数:9
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