Environmental Research Letters (Jan 2024)

Mesoscale eddies inhibit intensification of the Subantarctic Front under global warming

  • Dapeng Li,
  • Zhao Jing,
  • Wenju Cai,
  • Zhengguang Zhang,
  • Jiuxin Shi,
  • Xiaohui Ma,
  • Bolan Gan,
  • Haiyuan Yang,
  • Zhaohui Chen,
  • Lixin Wu

DOI
https://doi.org/10.1088/1748-9326/ad8173
Journal volume & issue
Vol. 19, no. 11
p. 114054

Abstract

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Oceanic mesoscale eddies are important dynamical processes in the Southern Ocean. Using high-resolution (∼0.1° for the ocean) Community Earth System Model (CESM-HR) simulations under a high-carbon emission scenario, we investigate the role of mesoscale eddies in regulating the response of the Subantarctic Front (SAF) to global warming. The CESM-HR simulates more realistic oceanic fronts and mesoscale eddies in the Southern Ocean than a coarse-resolution (∼1° for the ocean) CESM. Under global warming, the SAF is projected to intensify. The mean flow temperature advection intensifies the front, whereas the mesoscale-eddy-induced temperature advection and atmospheric dampening play primary (∼67%) and secondary (∼28%) roles in counteracting the effect of mean flow temperature advection. Our study suggests the importance of mesoscale eddies on inhibiting the SAF intensification under global warming and necessity of mesoscale-eddy-resolving simulations for faithful projection of future climate changes in the Southern Ocean.

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