Articles | Volume 25, issue 1
https://doi.org/10.5194/hess-25-375-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-25-375-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Jan 2021
Research article |
| 21 Jan 2021
| 21 Jan 2021
At which timescale does the complementary principle perform best in evaporation estimation?
Liming Wang
Department of Hydraulic Engineering, State Key Laboratory of
Hydroscience and Engineering, Tsinghua University, Beijing 100084, China
Songjun Han
State Key Laboratory of Simulation and Regulation of Water Cycle in
River Basin, China Institute of Water Resources and Hydropower Research,
Beijing 100038, China
Department of Hydraulic Engineering, State Key Laboratory of
Hydroscience and Engineering, Tsinghua University, Beijing 100084, China
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Cited
15 citations as recorded by crossref.
- Comparative evaluation of four actual evapotranspiration models over different ecosystems and climate zones in China M. Yuan et al. 10.2166/wcc.2024.724
- Combining the Generalized Complementary Relationship and the Modified Priestley-Taylor Equation to estimate and partition the evapotranspiration of typical plantations and grasslands in the Loess Plateau of China C. Fu et al. 10.1016/j.agwat.2023.108420
- The Evaporation on the Tibetan Plateau Stops Increasing in the Recent Two Decades L. Wang et al. 10.1029/2022JD037377
- Sigmoid Generalized Complementary Equation for Evaporation Over Wet Surfaces: A Nonlinear Modification of the Priestley‐Taylor Equation S. Han et al. 10.1029/2020WR028737
- Improving the Applicability of Lumped Hydrological Models by Integrating the Generalized Complementary Relationship X. Lei et al. 10.1029/2023WR035567
- Relations of rescaled to non-rescaled complementary models and improvement of evapotranspiration estimation by incorporating both climatic and land surface conditions Z. Mu et al. 10.1016/j.agwat.2024.108989
- Comparison of the Efficiencies of the Prognostic Generalized Complementary Functions on Evaporation Estimation L. Wang et al. 10.1029/2023JD038683
- Should two-parameter generalized complementary models for evaporation be simplified to single-parameter? A pairwise evaluation over grassland and forest sites S. Han et al. 10.1016/j.agrformet.2024.110209
- Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau C. Shang et al. 10.3390/rs14092047
- Contrasting Land and Atmospheric Controls on the Generalized Complementary Relationship of Evaporation Over Grasslands and Forests S. Han et al. 10.1029/2023WR035501
- Combining the FAO-56 method and the complementary principle to partition the evapotranspiration of typical plantations and grasslands in the Chinese Loess Plateau C. Fu et al. 10.1016/j.agwat.2024.108734
- Applicability of the complementary relationship of evapotranspiration for heterogeneous vegetation cover at boundary and plot scales C. Fu et al. 10.1016/j.ejrh.2024.102117
- Potential Evaporation and the Complementary Relationship Z. Tu et al. 10.1029/2022WR033763
- Connotation analysis of parameters in the generalized nonlinear advection aridity model H. Zhou et al. 10.1016/j.agrformet.2021.108343
- Comparison of formulating apparent potential evaporation with pan measurements and Penman methods L. Wang et al. 10.1016/j.jhydrol.2020.125816
14 citations as recorded by crossref.
- Comparative evaluation of four actual evapotranspiration models over different ecosystems and climate zones in China M. Yuan et al. 10.2166/wcc.2024.724
- Combining the Generalized Complementary Relationship and the Modified Priestley-Taylor Equation to estimate and partition the evapotranspiration of typical plantations and grasslands in the Loess Plateau of China C. Fu et al. 10.1016/j.agwat.2023.108420
- The Evaporation on the Tibetan Plateau Stops Increasing in the Recent Two Decades L. Wang et al. 10.1029/2022JD037377
- Sigmoid Generalized Complementary Equation for Evaporation Over Wet Surfaces: A Nonlinear Modification of the Priestley‐Taylor Equation S. Han et al. 10.1029/2020WR028737
- Improving the Applicability of Lumped Hydrological Models by Integrating the Generalized Complementary Relationship X. Lei et al. 10.1029/2023WR035567
- Relations of rescaled to non-rescaled complementary models and improvement of evapotranspiration estimation by incorporating both climatic and land surface conditions Z. Mu et al. 10.1016/j.agwat.2024.108989
- Comparison of the Efficiencies of the Prognostic Generalized Complementary Functions on Evaporation Estimation L. Wang et al. 10.1029/2023JD038683
- Should two-parameter generalized complementary models for evaporation be simplified to single-parameter? A pairwise evaluation over grassland and forest sites S. Han et al. 10.1016/j.agrformet.2024.110209
- Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau C. Shang et al. 10.3390/rs14092047
- Contrasting Land and Atmospheric Controls on the Generalized Complementary Relationship of Evaporation Over Grasslands and Forests S. Han et al. 10.1029/2023WR035501
- Combining the FAO-56 method and the complementary principle to partition the evapotranspiration of typical plantations and grasslands in the Chinese Loess Plateau C. Fu et al. 10.1016/j.agwat.2024.108734
- Applicability of the complementary relationship of evapotranspiration for heterogeneous vegetation cover at boundary and plot scales C. Fu et al. 10.1016/j.ejrh.2024.102117
- Potential Evaporation and the Complementary Relationship Z. Tu et al. 10.1029/2022WR033763
- Connotation analysis of parameters in the generalized nonlinear advection aridity model H. Zhou et al. 10.1016/j.agrformet.2021.108343
1 citations as recorded by crossref.
Latest update: 30 Mar 2025
Short summary
It remains unclear at which timescale the complementary principle performs best in estimating evaporation. In this study, evaporation estimation was assessed over 88 eddy covariance monitoring sites at multiple timescales. The results indicate that the generalized complementary functions perform best in estimating evaporation at the monthly scale. This study provides a reference for choosing a suitable time step for evaporation estimations in relevant studies.
It remains unclear at which timescale the complementary principle performs best in estimating...
