Abstract The cross-scale energy transfer among oceanic mesoscale eddies is crucial to shape their equilibrium state with important climate and ecological implications. The classical 2- and 3-dimensional turbulence theories predict an upscale and downscale energy transfer locally in spectral space (i.e., a cascade-like process), respectively. However, using unprecedented high-resolution measurements of sea level anomalies from the Surface Water and Ocean Topography (SWOT) mission combined with a high-resolution oceanic simulation, we demonstrate the coexistence of downscale and upscale transfers for surface mesoscale eddy kinetic energy (EKE) in the Southern Ocean. The latter dominates the former, leading to a net upscale surface EKE transfer. The downscale surface EKE transfer is generally local in the spectral space, achieved primarily via interactions of mesoscale eddies with horizontal scales differing by less than a factor of 2. In contrast, the upscale surface EKE transfer is less local, involving mesoscale eddies with larger horizontal scale separation. Accordingly, the upscale surface EKE transfer is severely underestimated in measurements from the last generation of satellite altimeters even at their well-resolved scales O(100 km). Our findings uncover the crucial contribution of EKE transfer by interactions among mesoscale eddies with evident scale differences, which is overlooked in the existing oceanography literature.
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