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Topographic Influences on Wind-Driven, Stratified Flow in a β-Plane Channel：An Idealized Model for the Antarctic Circumpolar Current
Topographic Influences Wind-Driven Stratified Flow β-Plane Channel Antarctic Circumpolar Current
2008/12/27
Topographic influences are examined in an eddy-resolving model of oceanic channel flow forced by steady zonal winds. With small explicit lateral friction, transient eddies generated by the baroclinic ...
On Stratified Flow over a Ridge Intersecting Coastlines
Stratified Flow Ridge Intersecting Coastlines circulation model
2008/12/24
The adjustment between two interconnecting basins of stratified fluid, resulting from the formation of a pool of dense water in one, is investigated with an 18-level numerical general circulation mode...
The evolution of a steady stratified along-isobath current flowing cyclonically (shallower water on the right looking downstream) over a sloping frictional bottom is examined using an idealized model....
Stratified Flow along a Corrugated Slope: Separation Drag and Wave Drag
Stratified Flow Corrugated Slope Separation Drag Wave Drag
2008/7/31
Lee wave generation and horizontal flow separation in stratified flow along a slope, with corrugations or a ridge running directly downslope, are explored using analytical and numerical methods. Both ...