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Transport into the extratropical lowermost stratosphere (LMS) can be divided into a slow part (time-scale of several months to years) associated with the global-scale stratospheric residual circulatio...
We describe the residual circulation induced in a two-layer system when internal waves, with a wave length equal to or longer than the slope length, propagate over a sloping bottom and either reflect ...
Many aspects Of the low-frequency response of a stratified inlet have not been previously observed because of the lack of simultaneous observations of runoff, wind, currents, and density over the enti...
The dynamics of the meridional overturning of the Antarctic Circumpolar Current (ACC) are best described in terms of a residual circulation that sums the transport of the wind-driven Ekman layer to th...

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