Preprints
https://doi.org/10.5194/essd-2025-463
https://doi.org/10.5194/essd-2025-463
14 Aug 2025
 | 14 Aug 2025
Status: this preprint is currently under review for the journal ESSD.

UEx-L-Eddies: Decadal and global long-lived mesoscale eddy trajectories with coincident air-sea CO2 fluxes and biogeochemical conditions

Daniel J. Ford, Jamie D. Shutler, Katy L. Sheen, Gavin H. Tilstone, and Vassilis Kitidis

Abstract. Mesoscale eddies are prevalent features within the global ocean that modify the physical, chemical and biological properties as they move and evolve. These modifications can alter the air-sea exchange of CO2, and therefore these features may be hotspots for enhanced or reduced CO2 uptake compared to the surrounding environment. The understanding of the global and regional effect of mesoscale eddies on ocean CO2 uptake is however limited and largely based on single eddies or small regional subsets. Here, we provide a global dataset of 5996 long lived eddies trajectories (lifetimes greater than a year) with corresponding air-sea CO2 fluxes all tracked using a Lagrangian approach between 1993 to 2022. The trajectories comprise 3244 anticyclonic (‘warm core’) and 2752 cyclonic (‘cold core’) eddies and the dataset provides the biogeochemical conditions, including the CO2 fluxes, within and outside each eddy. The dataset refines a previous regional methodology with a focus on climate quality environmental parameters and uses a global neural network for estimating the fugacity of CO2 in seawater (fCO2 (sw)) along with a comprehensive air-sea CO2 flux uncertainty budget. These refinements provide a robust foundation for studying the modulation of air-sea CO2 fluxes by mesoscale eddies. As an example use of the dataset, we investigate the role of mesoscale eddies in modifying the global and regional air-sea CO2 fluxes, by comparing the eddy driven air-sea CO2 flux to that of the surrounding environment. We find that globally, long-lived anticyclonic eddies enhanced the CO2 sink by 4.5 ± 2.8 % (95 % confidence), while long-lived cyclonic eddies reduce the CO2 sink by 0.7 ± 2.6 %. Collectively, the long-lived eddies indicate an enhancement of the ocean CO2 sink by 2.7 ± 1.1 Tg C yr-1. Propagating the air-sea CO2 flux uncertainties was found to be a key component needed to fully understand apparent differences between previous regional and global studies. The long lived eddies (UEx-L-Eddies) dataset is available on Zenodo at https://doi.org/10.5281/ZENODO.16355763 (Ford et al., 2025).

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Daniel J. Ford, Jamie D. Shutler, Katy L. Sheen, Gavin H. Tilstone, and Vassilis Kitidis

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Daniel J. Ford, Jamie D. Shutler, Katy L. Sheen, Gavin H. Tilstone, and Vassilis Kitidis

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UEx-L-Eddies: decadal and global long-lived mesoscale eddy trajectories with coincident air-sea CO2 fluxes and biogeochemical conditions (v0-2) D. J. Ford et al. https://doi.org/10.5281/ZENODO.16355763

Daniel J. Ford, Jamie D. Shutler, Katy L. Sheen, Gavin H. Tilstone, and Vassilis Kitidis

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Short summary
Mesoscale eddies are abundant in the global oceans affect the physical, chemical and biological properties of the ocean. These changes can modify the air-sea CO2 fluxes. Here, we present a dataset of air-sea CO2 fluxes for 5996 long lived mesoscale eddies trajectories in the global ocean between 1993 to 2022. These trajectories can be used to understand the processes modifying and controlling the air-sea CO2 fluxes in mesoscale eddies which are supported by a comprehensive uncertainty budget.
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