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Published on: July 14, 2023
A nutrient relay sustains subtropical ocean productivity.
Mukund Gupta1,2, Richard G Williams3, Jonathan M Lauderdale1
1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139.
Subtropical ocean gyres rely on mesoscale eddies and particle remineralization for nutrient replenishment. This nutrient relay sustains ocean productivity and carbon export in these vital marine ecosystems.
Area of Science:
- Oceanography
- Biogeochemistry
- Climate Science
Background:
- Subtropical ocean gyres are crucial for global carbon export.
- Nutrient replenishment in subeuphotic layers of gyres is poorly understood.
- Surface productivity depletes nutrients, necessitating resupply mechanisms.
Purpose of the Study:
- To quantify nutrient resupply mechanisms in subtropical ocean gyres.
- To investigate the role of mesoscale eddies in nutrient transport.
- To understand the pathways sustaining gyre productivity.
Main Methods:
- Utilized a global, eddy-permitting ocean physics and biogeochemistry simulation.
- Quantified nutrient fluxes along and across density surfaces.
- Assessed the contribution of mesoscale eddies (10-100 km) to nutrient transport.
Main Results:
- Mesoscale eddies transport nutrients from gyre flanks into the interior.
- Nutrient resupply to subeuphotic layers is equally driven by eddy transport and particle remineralization.
- Eddy-driven nutrient supply is significant in the lower thermocline and dominant within gyre interiors.
Conclusions:
- Subtropical gyre productivity is sustained by a nutrient relay system.
- Lateral nutrient transport by eddies is critical for thermocline resupply.
- This process supports surface biological production and carbon export.
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