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Residual circulation trajectories and transit times into the extratropical lowermost stratosphere
the extratropical lowermost stratosphere residual circulation trajectories
2011/2/24
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...
Residual circulation due to internal waves shoaling on a slope
Residual circulation internal waves shoaling a slope
2014/4/17
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 ...
The Low-Frequency Residual Circulation in Knight Inlet, British Columbia
Low-Frequency harmonic analysis Knight Inlet
2008/12/11
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...
Constructing the Residual Circulation of the ACC from Observations
Residual Circulation ACC Observations
2008/6/26
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...