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Peter Rhines and I worked on the eddy dynamics of deep water flow across the Antarctic Circumpolar Current (ACC), and its relation to bottom topographic form stress. This is a large numerical modeling effort, using an idealized geometry and a novel analysis scheme. We have analyzed the poleward flux of mass between density surfaces due to eddies. We orient the flux calculations to be along the curving paths of the time-mean geostrophic flow, which has a fixed spatial structure due to the bottom topography. We find that the eddy transports across these paths are localized within the strong eddy-energy regions in the lee of topographic features (MacCready and Rhines, 2001). This result has been suggested before, but never seen in numerical analyses, due to the difficulty of working on arbitrary curved paths. At the left is are numerical results, showing the time-mean meridional transport due to eddy geostrophic bolus flux normal to the time mean upper layer geostrophic streamfunction. |