Toward More Accurate Modeling of Canopy Radiative Transfer and Leaf Electron Transport in Land Surface Modeling
Abstract
Modeling leaf photosynthesis is essential for quantifying the carbon, water, and energy fluxes of the terrestrial biosphere. However, due to the lack of simultaneous measurements of leaf light absorption and gas exchange, canopy radiative transfer (RT) and photosynthesis modeling often rely on simplified assumptions about light absorption and electron transport. These assumptions ignore variations in leaf biophysical traits and environmental conditions. In this study, we utilized a next-generation land surface model (LSM)—CliMA Land, which incorporates hyperspectral canopy RT and provides a more accurate representation of trait variations. We evaluated the potential bias in electron transport estimates introduced by the broadband RT schemes used in traditional LSMs. Additionally, we explored the impact of different leaf electron transport parameterization schemes on global-scale photosynthesis and fluorescence modeling. We showed that (a) traditional LSMs that disregard the impacts of leaf temperature and leaf traits on electron transport tend to overestimate electron transport rates. (b) Photosynthesis and fluorescence within a grid can exhibit biases exceeding 20%, with these biases demonstrating contrasting seasonality. (c) Global estimates of integrated photosynthesis and fluorescence differ by 8.1% and 8.8%, respectively. These results underscore the importance of adopting more sophisticated and accurate modeling schemes, such as hyperspectral canopy RT, in future LSMs and Earth system modeling to enhance the reliability of modeling outcomes.
Copyright and License
© 2024 The Authors. Journal of Advancesin Modeling Earth Systems published by Wiley Periodicals LLC on behalf ofA merican Geophysical Union. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
Acknowledgement
This research has been supported by the National Aeronautics and Space Administration (NASA) Carbon Cycle Science Grant 80NSSC21K1712 and OCO 2/3 Science Team Grant 80NSSC21K1075 awarded to Christian Frankenberg.
Contributions
Conceptualization: Yujie Wang
Data curation: Yujie Wang
Formal analysis: Yujie Wang, Christian Frankenberg
Funding acquisition: Christian Frankenberg
Investigation: Yujie Wang, Christian Frankenberg
Methodology: Yujie Wang, Christian Frankenberg
Project administration:Christian Frankenberg
Software: Yujie Wang
Supervision: Christian Frankenberg
Validation: Yujie Wang
Data Availability
We coded our model and did the analysis using Julia (version 1.10.0). The leaf level and global scale simulations were done using CliMA Land, which is available from the project website: https://github.com/CliMA/Land under the Apache 2.0 License. The exact version of the model used to produce the results used in this paper is archived on Zenodo (Wang & Frankenberg, 2024a). The global CliMA Land simulation with a tag of “a11_gm3_wd1” can be found at Wang and Frankenberg (2024b).
Conflict of Interest
The authors declare no conflicts of interest relevant to this study.
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Additional details
- ISSN
- 1942-2466
- National Aeronautics and Space Administration
- 80NSSC21K1712
- National Aeronautics and Space Administration
- 80NSSC21K1075
- Caltech groups
- Division of Geological and Planetary Sciences