搜索结果: 1-15 共查到“海洋科学 Boundary Currents”相关记录22条 . 查询时间(0.062 秒)
Some simple momentum advection effects are considered in a current aligned with the y axis on which there is superimposed a "cross" flow in the x-z plane. The cross flow coupled with horizontal shear ...
Baroclinic Boundary Currents and Long Edge-Waves in Basins with Sloping Shores
Baroclinic Boundary Currents Sloping Shores Long Edge-Waves
2009/3/9
Earlier work on baroclinic “coastal jets” and Kelvin waves in constant-depth basins is extended to basins with sloping shores. Baroclinic coastal jets are again found to be set up by an inflow or outf...
Eastern Boundary Currents and Coastal Upwelling
Eastern Boundary Currents Coastal Upwelling
2009/2/8
The adjustment of the eastern coastal zone of an inviscid ocean with vertical walls to a change in wind conditions occurs in two stages. After the propagation of a Kelvin wave across the forced region...
Potential Vorticity Dynamics of Boundary Currents in a Quasi-geostrophic Ocean
Vorticity Dynamics Quasi-geostrophic Ocean Boundary Currents
2009/1/4
Boundary layer potential vorticity dynamics for a quasi-geostrophic, eddy-resolving general circulation ocean model are studied using both Lagrangian and Eulerian analyses. Active western boundary lay...
Boundary Currents, Free Currents and Dissipation in the Low-Frequency Scattering of Shelf Waves
Boundary Currents Low-Frequency Scattering Free Currents
2009/1/4
The low-frequency scattering of barotropic shelf waves is considered in the limit of small but nonzero dissipation. For a rectilinear shelf it is shown that an intense oscillatory boundary layer forms...
Potential Vorticity Sources and Sinks in a Quasi-geostrophic Ocean：beyond Western Boundary Currents
eddy-resolving general circulation model Potential Vorticity Sources Quasi-geostrophic Ocean
2008/12/30
Potential vorticity dynamics for a quasi-geostrophic eddy-resolving general circulation model (EGCM) are studied in order to determine the effects of mesoscale variability on the potential vorticity d...
Matching a Ventilated Thermocline Model with Inertial Western Boundary Currents
Ventilated Thermocline Model Inertial Western Boundary Currents western boundary region
2008/12/30
A two-layered ventilated thermocline model is matched with inertial western boundary currents in the southern part of the western boundary region. For general cases the western boundary currents break...
Countergradient vorticity Flux Generated in Continental Boundary Currents
Continental Boundary Currents Countergradient vorticity Flux
2008/12/24
It is suggested that the inshore shear of continental boundary flows like the Florida Current can be accounted for by a countergradient vorticity flux, rather than by lateral diffusion to the shore. T...
The Link between Western Boundary Currents and Equatorial Undercurrents
Equatorial Undercurrent Western Boundary Currents
2008/12/24
A constant potential vorticity model is used to investigate the relation between the properties of an equatorward-directed western boundary current and the formation of the Equatorial Undercurrent (EU...
Nonlinear Disturbances of Western Boundary Currents
Nonlinear Disturbances Western Boundary Currents
2008/12/19
Viscous shear instability is proposed as a primary mechanism for generating time-dependent eddies at western boundaries. Thus, the authors examine the stability of the Munk flow with constant transpor...
The Influence of Layer Outcropping on the Separation of Boundary Currents. Part I：The Wind-driven Experiments
zero wind-stress curl line Layer Outcropping Wind-driven Experiments
2008/12/18
The influence of outcropping isopycnal layers on the separation of western boundary currents is investigated in a series of wind-driven eddy-resolving multilayer primitive equation numerical experimen...
On the Role of Dissipation in Inertial Western Boundary Currents
Inertial Western Boundary Currents western boundary layer
2008/12/17
The problem of matching the nonlinear, frictional flow in a simple western boundary layer to a specified interior flow is considered. Two problems are discussed, using streamfunction as a coordinate a...
The Asymmetry of Western Boundary Currents in the Upper Atlantic Ocean
western boundary current Upper Atlantic Ocean
2008/12/15
Observations of upper-ocean western boundary current (WBC) transports reveal asymmetries between the Northern and the Southern Hemispheres of the Atlantic Ocean. To find out what mechanism might cause...
The Influence of Layer Outeropping on the Separation of Boundary Currents. Part II：The Wind- and Buoyancy-Driven Experiments
Layer Outeropping Wind-and Buoyancy-Driven Experiments Boundary Currents
2008/12/12
It is shown that the main characteristic of the Persons western boundary current separation mechanism, namely a separation south of the zero wind stress curt line (ZWCL), is no longer present when dia...
Vorticity Dissipation by Western Boundary Currents in the Presence of Outcropping Layers
Vorticity Dissipation Outcropping Layers Western Boundary Currents
2008/12/11
In an exploration of the dynamics of current separation and vorticity dissipation in a two-layer model, the following is found. 1) Results obtained in a barotropic context remain valid; namely, two ma...
