2026/02/28 by Takuro Matsuta, Yuki Tanaka, Atsushi Kubokawa
Earth and Planetary Sciences · Environmental Science · #Oceanographic and Atmospheric Processes #Tropical and Extratropical Cyclones Research #Climate variability and models
paper · doi:10.1175/jpo-d-25-0220.1
Abstract The transport of the Antarctic Circumpolar Current (ACC) has been shown to increase with friction. Previous studies explained this counterintuitive relationship called frictional control based on the eddy geometric parameterizations. They focused on the eddy momentum transfer and eddy energetics. To maintain the balance between wind stress and eddy interfacial form stress, eddy energy must remain unchanged as friction increases; this requires enhanced baroclinicity to compensate for stronger eddy energy dissipation. However, the independence of eddy energy has not been fully verified, and this interpretation assumes negligible barotropic energy conversion. To address this gap, we conduct sensitivity experiments in an idealized stratified reentrant channel with varying linear bottom drag. Numerical simulations show that eddy energy changes substantially with friction. Furthermore, in the high-drag regime, baroclinic energy conversion dominates eddy energy generation, whereas in the low-drag regime, barotropic energy conversion contributes substantially. Despite these differences, baroclinicity increases with eddy energy dissipation across all regimes, although the relationship is somewhat weak in the low-drag regime owing to barotropic energy conversion. To explain this phenomenon, we extend the frictional control framework based on the Lorenz energy cycle. A simple scaling argument leads to a generalized frictional control, s ∼ D ( E )/ τ w , where s is the baroclinicity, D ( E ) is the eddy energy dissipation, and τ w is the wind stress. This framework provides a natural extension of the existing framework and successfully explains the numerical results. These results indicate that eddy dissipation controls the baroclinicity; therefore, properly parameterizing the eddy dissipation rate is essential for representing ACC dynamics in ocean models.