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Transient overturning changes cause an upper-ocean nutrient decline in a warming climate

Author

Listed:
  • Shantong Sun

    (Laoshan Laboratory
    Florida State University
    California Institute of Technology)

  • Andrew F. Thompson

    (California Institute of Technology)

  • Jimin Yu

    (Laoshan Laboratory
    Australian National University
    Chinese Academy of Sciences)

  • Lixin Wu

    (Laoshan Laboratory
    Ocean University of China)

Abstract

Models and proxy data suggest multi-centennial nutrient reorganization and biological productivity changes under sustained climate warming. These changes have traditionally been attributed to processes in the Southern Ocean. Here we instead show that transient overturning circulation adjustments, associated with changes in the Atlantic Meridional Overturning Circulation (AMOC), dominate the global nutrient reorganization on centennial timescales. Following an AMOC weakening, a typical feature of a warming climate, a transient overturning circulation develops in the Indo-Pacific basins, characterized by enhanced southward transport in the deep ocean. Coupled with the vertical nutrient structure, these transient overturning changes produce a net transport of nutrients from the Indo-Pacific into the Southern Ocean. Meanwhile, isopycnal surfaces deepen and bring nutrient-depleted waters to greater depths, causing nutrient concentrations to decline in much of the global upper ocean. Given the close link between nutrients and carbon, our findings suggest that transient overturning circulation changes across different basins can critically affect the marine carbon cycle.

Suggested Citation

  • Shantong Sun & Andrew F. Thompson & Jimin Yu & Lixin Wu, 2024. "Transient overturning changes cause an upper-ocean nutrient decline in a warming climate," Nature Communications, Nature, vol. 15(1), pages 1-9, December.
    • Handle: RePEc:nat:natcom:v:15:y:2024:i:1:d:10.1038_s41467-024-52200-0
    DOI: 10.1038/s41467-024-52200-0
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    References listed on IDEAS

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    2. Andreas Schmittner, 2005. "Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation," Nature, Nature, vol. 434(7033), pages 628-633, March.
    3. L. Menviel & P. Spence & J. Yu & M. A. Chamberlain & R. J. Matear & K. J. Meissner & M. H. England, 2018. "Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise," Nature Communications, Nature, vol. 9(1), pages 1-12, December.
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