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Serguei Sokolov and Stephen R. Rintoul

waves (not shown). The fact that Fig. 4 shows these gradient maxima cluster around a particular SSH value suggests that such features have a preferred propagation path (in SSH space). e. Frequency distributions of the frontal pattern Having demonstrated that the fronts of the Southern Ocean can be traced reliably using SSH, we now use the weekly time series of SSH maps to characterize the variability of the ACC fronts in space and time. Variability in the path of the frontal jets is shown in Fig

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