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Updated: Sep 3, 2025

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
Published on: June 24, 2019
Reconciling carbon-cycle processes from ecosystem to global scales
Ashley P Ballantyne1,2, Zhihua Liu3, William Rl Anderegg4
1Department of Ecosystem and Conservation Sciences University of Montana Missoula MT.
Estimating carbon (C) dynamics is challenging due to disagreements in C-cycle process data. Combining satellite, atmospheric, and terrestrial/aquatic data can reconcile spatial mismatches and improve C-cycle science.
Area of Science:
- Ecology
- Earth Science
- Environmental Science
Background:
- Global carbon (C) dynamics understanding is a significant scientific challenge.
- Expansion of carbon dioxide (CO2) observatories enables C-cycle process estimation but reveals data discrepancies.
- Ecosystem-specific C retention varies widely, with grasslands retaining 2% and needleleaf forests 30% of fixed C.
Purpose of the Study:
- To reconcile spatial mismatches in C-cycle process estimates across scales.
- To identify potential carbon loss pathways using novel data integration.
- To advance C-cycle science across the land-water interface.
Main Methods:
- Utilizing newly available satellite and atmospheric data.
- Combining independent datasets from terrestrial and aquatic environments.
- Comparing ecosystem measurements with continental-scale estimates.
Main Results:
- Continental US scale net ecosystem exchange (NEE) accounts for only 5% of photosynthetically fixed C.
- Significant spatial mismatches exist, with the Southeast showing high gross primary productivity and the Midwest high NEE.
- Ecosystem measurements reveal substantial variations in C retention across different biomes.
Conclusions:
- Innovative integration of diverse datasets is crucial for accurate C-cycle assessments.
- Addressing spatial mismatches is key to improving global carbon budget estimations.
- Integrating land and water C-cycle science provides a more holistic understanding of global C dynamics.
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