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A Numerical Study on the Role of Mesoscale Cold-Core Eddy in Modulating the Upper Ocean Responses to Typhoon Trami (2018).


With two groups of numerical experiments with and without the cold-core eddy (CCE), the impacts of the CCE on the upper ocean responses to Typhoon Trami (2018) were investigated using a coupled atmosphere-ocean model. It’s commonly accepted that the CCE promotes the sea surface cooling (SSC) primally through the enhanced vertical mixing, while the contributions from the wind-driven advection and the near-inertial advection to the differences in the sea surface temperature (dSST) were underestimated. This study found that the presence of CCE contributed to the stronger along-track cold advection, which dominated the increase in the SSC near the radius of maximum wind (RMW) to the right of Trami’s track, and the stronger cross-track warm advection was acting to prevent the cooling induced by the vertical mixing. During the relaxation stage, the stronger near-inertial advection within the CCE accounted largely for the amplification and the redistribution of the dSST. As for the dynamic responses, the enhanced upwelling and downwelling within the CCE explained the larger cooling and warming in the sub-surface temperature oscillations. The wind-driven acceleration of the currents in the mixing layer was larger during the typhoon-eddy interaction so that the CCE became an efficient mixer, thus contributing to the rapid surfacing of the cold water and the ensuing stronger wind-driven advection. These results highlight the importance of the advection processes in the modulating effect of the CCE. Therefore, 3D ocean models are needed to incorporate the mesoscale features of the oceanic eddies for realistically reproducing the upper ocean responses to tropical cyclones (TCs).