Journal
AGRICULTURAL AND FOREST METEOROLOGY
Volume 315, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.agrformet.2021.108790
Keywords
Carbon dioxide fluxes; Eddy Covariance; Evapotranspiration; Flux partitioning; Photosynthesis; Respiration
Categories
Funding
- Moore Charitable Foundation Science-to-Action Fund from the School of Engineering and Applied Science at Princeton
- Army Research Office [W911NF2010216]
- NSF [DEB 1802885]
- U.S. National Science Foundation [NSF-AGS-1644382, NSF-AGS-2028633, NSF-IOS-1754893, NSF-AGS-0955444]
- European Research Council (ERC) under the European Unions Horizon 2020 research and innovation programme [724629]
- Brazils National Research Council (CNPq) research scholarship [301420/2017-3]
- E. & J. Gallo Winery
- NASA Applied Sciences-Water Resources Program [NNH17AE39I]
- National Natural Science Foundation of China [41875013]
- U.S. Department of Defense (DOD) [W911NF2010216] Funding Source: U.S. Department of Defense (DOD)
- European Research Council (ERC) [724629] Funding Source: European Research Council (ERC)
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The partitioning of evapotranspiration and net ecosystem exchange into different components is crucial for understanding water cycle and carbon dioxide exchange. Different methods, including partitioning models and similarity-based approaches, have been evaluated and compared to provide insights into their strengths and weaknesses.
The partitioning of evapotranspiration (ET) into surface evaporation (E) and stomatal-based transpiration (T) is essential for analyzing the water cycle and earth surface energy budget. Similarly, the partitioning of net ecosystem exchange (NEE) of carbon dioxide into respiration (R) and photosynthesis (P) is needed to quantify the controls on its sources and sinks. Promising approaches to obtain these components from field measurements include partitioning models based on analysis of conventional high frequency eddy-covariance data. Here, two such existing approaches, based on similarity between non-stomatal (R and E) and stomatal (P and T) components, are considered: the Modified Relaxed Eddy Accumulation (MREA) and Flux-Variance Similarity (FVS) models. Moreover, a simpler technique is proposed based on a Conditional Eddy-Covariance (CEC) scheme. All approaches were evaluated against independent estimates of transpiration and respiration. The CEC method agreed better with measurements of transpiration over a grass field, with a smaller root mean square error (5.9 W m(-2)) and higher correlation (0.96). At a forest site, better agreement with soil respiration was found for FVS above the canopy, while CEC and MREA performed better below the canopy. Further application of these methods over a vineyard and a pine forest across different seasons provided insight into the main strengths and weaknesses of each approach. FVS and MREA converge less often when ground flux components dominate, while CEC might result in noisy P and R for small NEE. Finally, in the CEC and MREA framework, the ratio T/ET is shown to be related to the correlation coefficient for carbon dioxide and water vapor concentrations, which can thus be used as a qualitative measure of the importance of stomatal and non-stomatal components. Overall, these results advance the understanding of the skill and agreement of all three methods, and inform future studies where the various approaches can be applied simultaneously and intercompared.
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