A5047429440- Plant Water Relations and Carbon Dynamics
- Hydrology and Watershed Management Studies
- Climate variability and models
- Solar and Space Plasma Dynamics
- Greenhouse Technology and Climate Control
- Heat Transfer and Optimization
- Scientific Research and Discoveries
- Hydrology and Drought Analysis
- Geophysics and Gravity Measurements
- Meteorological Phenomena and Simulations
University of Chinese Academy of Sciences
2023-2024
Institute of Soil and Water Conservation
2023-2024
Northwest A&F University
2023
The estimation of actual evapotranspiration (ET) using both rescaled and non-rescaled complementary relationship (CR) models has become a hotspot in the research on terrestrial ET. This study explores between these two CR improves method for calculating xmin models. can be functionally interconvertible, i.e., model enables simulation ET also conduct simulation. parameter b or c plays role similar to Based data from 15 catchments Loess Plateau China, we validate this Meanwhile, evaluate...
Land-surface evapotranspiration (ET) is a major component of the hydrologic cycle. It very attractive approach to estimate land surface ET by means complementary relationship (CR). After 60 years continuous exploration, CR has developed from linear relationships present nonlinear ones. There are usually four boundary conditions (BCs) for CR, among which first-order one in completely wet environments (dy/dxx=1) been debatable issue, including both difference values dy/dxx=1, and divergence...