Topographic control of basin and channel flows: the role of the bottom pressure torques and friction
Jackson, Laura; Hughes, Chris W.; Williams, Richard G.. 2006 Topographic control of basin and channel flows: the role of the bottom pressure torques and friction. Journal of Physical Oceanography, 36 (9). 1786-1805. 10.1175/JPO2936.1Full text not available from this repository.
The topographical control of western boundary currents within a basin and zonal jets in a channel is investigated in terms of the potential vorticity (PV) and barotropic vorticity (BV: the curl of the depth-integrated velocity) budgets using isopycnic, adiabatic wind-driven experiments. Along the western boundary, the wind-driven transport is returned across latitude lines by the bottom pressure torque, while friction is only important in altering the PV within an isopycnic layer and in allowing a closed circulation. These contrasting balances constrain the geometry of the flow through integral relationships for the BV and PV. For both homogenous and stratified basins with sloping sidewalls, the northward subtropical jet separates from the western wall and has opposing frictional torques on either side of the jet, which cancel in a zonal integral for BV but alter the PV within a layer streamline. In a channel with partial topographic barriers, the bottom pressure torque is again important in returning wind-driven flows along western boundaries and in transferring BV from neighboring wind-driven gyres into a zonal jet. The depth-integrated flow steered by topography controls where the bottom friction alters the PV, which can lead to different PV states being attained for separate subbasins along a channel.
|Format Availability:||Electronic, Print|
|Additional Keywords:||ANTARCTIC CIRCUMPOLAR CURRENT, POTENTIAL VORTICITY, SOUTHERN-OCEAN, CIRCULATION, MODEL, BALANCE, EDDIES|
|NORA Subject Terms:||Marine Sciences|
|Date made live:||01 Aug 2007 09:11|
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