2024
DOI: 10.1016/j.ejrh.2024.101653
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Exploring evapotranspiration stress in China: A blending approach employing multi-source remote sensing proxies

Yuan Liu,
Yong Zhao,
Jiaqi Zhai
et al.
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Cited by 1 publication
(2 citation statements)
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“…where ET ins is instantaneous evapotranspiration (mm/hr), λ is the latent heat of evapotranspiration (J/kg), and the number 3600 is the time conversion factor from seconds to hours. After calculating ET ins , the reference ET fraction is calculated using Equation (9). Then, the actual daily evaporation is obtained by multiplying the reference ET fraction by the daily ET value of the reference plant (Equation ( 10)).…”
Section: Calculation Of Instantaneous and Daily Evapotranspirationmentioning
confidence: 99%
See 1 more Smart Citation
“…where ET ins is instantaneous evapotranspiration (mm/hr), λ is the latent heat of evapotranspiration (J/kg), and the number 3600 is the time conversion factor from seconds to hours. After calculating ET ins , the reference ET fraction is calculated using Equation (9). Then, the actual daily evaporation is obtained by multiplying the reference ET fraction by the daily ET value of the reference plant (Equation ( 10)).…”
Section: Calculation Of Instantaneous and Daily Evapotranspirationmentioning
confidence: 99%
“…Traditional methods of measuring ET (e.g., lysimeter, eddy covariance, Bowen's ratio, FAO 56) are generally complex, costly, time-consuming, and point based [5,6]. Satellite data and remote sensing methods are increasingly employed for indirect ET measurements [7][8][9][10]. These data offer broad coverage, capturing heterogeneity and changes, while remaining cost-effective and featuring suitable time sequences and computer processing capabilities [11].…”
Section: Introductionmentioning
confidence: 99%