1188 / 2024-09-20 16:13:12
Mesoscale eddies inhibit intensification of the Subantarctic Front under global warming
mesoscale oceanic eddy,eddy-resolving climate simulations,global warming,the subantractic front
Session 35 - Eddy variability in the ocean and atmosphere: dynamics, parameterization and prediction
Abstract Accepted
Mesoscale oceanic 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.