The Contribution of Submesoscale over Mesoscale Eddy Iron Transport in the Open Southern Ocean

Takaya Uchida (1) , Dhruv Balwada (2) , Ryan P. Abernathey (3) , Galen Mckinley (3) , K. Shafer Smith (2) , Marina Lévy (4)

1 Department of Earth and Environmental Sciences [New York]
2 LDEO - Lamont-Doherty Earth Observatory
3 CAOS - Center for Atmosphere Ocean Science [NYU]
4 PROTEO - Processus et interactions de fine échelle océanique

Biological productivity in the Southern Ocean is limited by iron availability. Previous studies of iron supply have focused on mixed‐layer entrainment and diapycnal fluxes. However, the Southern Ocean is a region highly energetic mesoscale and submesoscale turbulence. Here we investigate the role of eddies in supplying iron to the euphotic zone, using a flat‐bottom zonally re‐entrant model, configured to represent the Antarctic Circumpolar Current region, that is coupled to a biogeochemical model with a realistic seasonal cycle. Eddies are admitted or suppressed by changing the model's horizontal resolution. We utilize cross spectral analysis and the generalized Omega equation to temporally and spatially decompose the vertical transport attributable to mesoscale and submesoscale motions. Our results suggest that the mesoscale vertical fluxes provide a first‐order pathway for transporting iron across the mixing‐layer base, where diapycnal mixing is weak, and must be included in modeling the open‐Southern Ocean iron budget.

Domaines: Géophysique [physics.geo-ph]

Takaya Uchida, Dhruv Balwada, Ryan P. Abernathey, Galen Mckinley, K. Shafer Smith, et al.. The Contribution of Submesoscale over Mesoscale Eddy Iron Transport in the Open Southern Ocean. Journal of Advances in Modeling Earth Systems, 2019, 11 (12), pp.3934-3958. ⟨10.1029/2019MS001805⟩. ⟨hal-02422867⟩