Relations of rescaled to non-rescaled complementary models and improvement of evapotranspiration estimation by incorporating both climatic and land surface conditions
文献类型:期刊论文
作者 | Mu, Zhaotao5,6,7; Liu, Wenzhao3,4,5,6,7; Ma, Ning2; Cheng, Changwu4,5,6,7; Zhou, Haixiang1 |
刊名 | AGRICULTURAL WATER MANAGEMENT
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出版日期 | 2024-09-01 |
卷号 | 302页码:12 |
关键词 | Land surface evapotranspiration Complementary relationship Model parameter Rescaled variable Loess Plateau Ecohydrology |
ISSN号 | 0378-3774 |
DOI | 10.1016/j.agwat.2024.108989 |
产权排序 | 6 |
英文摘要 | The accurate quantification of actual evapotranspiration (ET) is crucial for water resources management in agricultural production and ecological construction. Estimating ET using both rescaled and non-rescaled complementary relationship (CR) models has become a hotspot in the research on terrestrial ET. This study explores the relationship between these two CR models and improves the method for calculating xmin, which is the value of the independent variable x when the dependent variable y is equal to zero in rescaled CR models. The rescaled and non-rescaled CR models can be functionally interconvertible, i.e., the non-rescaled CR model enables the rescaled simulation of ET and the rescaled CR model can also conduct a non-rescaled simulation. The parameter b or c in the non-rescaled CR models plays a role similar to xmin in the rescaled models and vice versa. Based on the data from 15 catchments in the Loess Plateau of China, we validate this relationship between two CR models. Meanwhile, we evaluate the formulation for xmin proposed by Crago et al. (2016) (xmin-d) and the results show that the range of variation for xmin-d values is smaller than that for the xmin values obtained by inverse method from the models (xmin-i) in the interannual process. The mean xmin-i value of RCR-C2016 is larger than that of RCR-S2017, while the mean xmin-d value is in between these two values. The empirical function for xmin is developed using the aridity index (AI) and normalized difference vegetation index (NDVI) as independent variables in the interannual fluctuations. The empirical function for xmin is expressed only using the AI in the spatial variations at a mean annual scale. Cross-validation results show that the rescaled CR models with the empirical functions of xmin can more accurately estimate ET and simulate its interannual and spatial changes. |
WOS关键词 | WATER-USE EFFICIENCY ; LOESS PLATEAU ; TERRESTRIAL EVAPOTRANSPIRATION ; HYDROLOGICAL RESPONSES ; LANDSCAPE EVAPORATION ; CALIBRATION-FREE ; GROWING-SEASON ; VARIABILITY ; VEGETATION ; PRINCIPLE |
资助项目 | National Natural Science Foundation of China[41971049] ; CAS Youth Innovation Promotion Association[2023059] ; CAS Youth Innovation Promotion Association[2022RC003] |
WOS研究方向 | Agriculture ; Water Resources |
语种 | 英语 |
WOS记录号 | WOS:001294504500001 |
出版者 | ELSEVIER |
资助机构 | National Natural Science Foundation of China ; CAS Youth Innovation Promotion Association |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/209164] ![]() |
专题 | 陆地水循环及地表过程院重点实验室_外文论文 |
通讯作者 | Liu, Wenzhao |
作者单位 | 1.Northwest Normal Univ, Coll Geog & Environm Sci, Lanzhou 730070, Gansu, Peoples R China 2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China 3.Northwest A&F Univ, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess Pl, Yangling 712100, Shaanxi, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 5.Chinese Acad Sci & Minist Water Resources, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China 6.Minist Educ, Yangling 712100, Shaanxi, Peoples R China 7.Chinese Acad Sci, Res Ctr Soil & Water Conservat & Ecol Environm, State Key Lab Soil Eros & Dryland Farming Loess Pl, Yangling 712100, Shaanxi, Peoples R China |
推荐引用方式 GB/T 7714 | Mu, Zhaotao,Liu, Wenzhao,Ma, Ning,et al. Relations of rescaled to non-rescaled complementary models and improvement of evapotranspiration estimation by incorporating both climatic and land surface conditions[J]. AGRICULTURAL WATER MANAGEMENT,2024,302:12. |
APA | Mu, Zhaotao,Liu, Wenzhao,Ma, Ning,Cheng, Changwu,&Zhou, Haixiang.(2024).Relations of rescaled to non-rescaled complementary models and improvement of evapotranspiration estimation by incorporating both climatic and land surface conditions.AGRICULTURAL WATER MANAGEMENT,302,12. |
MLA | Mu, Zhaotao,et al."Relations of rescaled to non-rescaled complementary models and improvement of evapotranspiration estimation by incorporating both climatic and land surface conditions".AGRICULTURAL WATER MANAGEMENT 302(2024):12. |
入库方式: OAI收割
来源:地理科学与资源研究所
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