搜索结果: 1-14 共查到“continuously stratified”相关记录14条 . 查询时间(0.078 秒)
Upwelling and Coastal Jets in a Continuously Stratified Ocean
Coastal Jets Continuously Stratified Ocean Upwelling
2009/4/2
A simple, linear, two-dimensional, f-plane model of coastal upwelling in a continuously stratified ocean is investigated. The transient response of the fluid to an impulsively applied alongshore wind ...
Coastal-Trapped Waves in a Continuously Stratified Ocean
Coastal-Trapped Waves Continuously Stratified Ocean
2009/3/7
The theory of coastal-trapped waves is extended to include the general features of continuous density stratification, variable bottom topography, and a finite coastal wall. In the limit of a vanishing...
Continuously Stratified Models of the Steady-State Equatorial Ocean
Stratified Models Steady-State Equatorial Ocean
2009/2/9
Two linearized, vertically diffusive steady-state models are formulated on an equatorial β-plane. The purpose is (a) to investigate the vertical boundary-layer structure in a continuously stratified o...
On the Propagation of Isolated Multilayer and Continuously Stratified Eddies
Isolated Multilayer Integra expressions Continuously Stratified Eddies
2009/1/12
Integra expressions are derived for the east-west velocity of propagation of isolated eddies on a beta plane. It is assumed that the eddies have no surface or floor expression, i.e., that both surface...
A Continuously Stratified Nonlinear Ventilated Thermocline
Nonlinear Ventilated Thermocline subtropical gyre fluid thermocline equations
2009/1/9
Three exact, closed-form analytical solutions for the subtropical gyre are presented for the ideal fluid thermocline equations. Specifically, the flow is exactly geostrophic, hydrostatic, and mass and...
Solitons in a Continuously Stratified Equatorial Ocean
vertical stratification Pacific Ocean
2009/1/7
The equatorial soliton studies of Boyd are extended to include the effects of continuous vertical stratification. We use vertical profiles of density measured in the equatorial Pacific Ocean and an id...
Coastal-Trapped Waves in Continuously Stratified Channels. Part I：Numerical Description of Behavioral Properties
coastal-trapped wave Coastal-Trapped Waves Stratified Channels
2009/1/5
A numerical model which solves the linearized, quasi-geostrophic potential vorticity equation is used to describe free subinertial coastal-trapped wave (CTW) properties in channels with variable depth...
A Continuously Stratified Thermocline Model Incorporating a Mixed Layer of Variable Thickness and Density
continuously stratified thermocline model variable depth
2008/12/24
A continuously stratified, steady thermocline model is formulated in which a mixed layer of variable depth and density overlies a stratified thermocline. Rather than prescribe the distribution of dens...
Stationary Shock Fronts in a Continuously Stratified Thermocline Model
Stationary Shock Fronts Thermocline Model
2008/12/12
Fronts are ubiquitous in the ocean. Recent work by Dewar has considered the formation of oceanic fronts in a simple layered model.
In this contribution, the position and structure of similar fronts...
The Effect of Current-Induced Stress Perturbation On Baroclinic Rossby Waves in a Continuously Stratified Model
Current-Induced Stress Perturbation Baroclinic Rossby Waves Continuously Stratified Model
2008/12/11
A shear stress at the air–sea interface is induced by the presence of surface currents. In the case of isotropic wind, a quadratic stress law leads to a stress curl proportional to and opposing the su...
Unsteady Abyssal Circulation Driven by a Discrete Buoyancy Source in a Continuously Stratified Ocean
Circulation Driven Discrete Buoyancy Source Stratified Ocean
2008/11/24
Analytical and numerical models are presented for linear quasigeostrophic buoyancy-driven flow forced bya time periodic pulsating point mass source in a continuously stratified, incompressible β-plane...
Evolution of Long Planetary Wave Packets in a Continuously Stratified Ocean
Long Planetary Wave Continuously Stratified Ocean
2008/7/2
Recent TOPEX/Poseidon observations show an enhanced (weakened) westward propagation of long planetary Rossby waves at extratropics (Tropics) and they usually propagate faster in the western basin than...
Climate Variability Inferred from a Continuously Stratified Model of the Ideal-Fluid Thermocline
Climate Variability Inferred Continuously Stratified Model Ideal-Fluid Thermocline
2008/6/30
Climate variability in the subtropical gyre interior induced by anomalous surface thermal forcing, Ekman pumping, mixed layer depth variability, and anomalous subpolar water formation is examined, usi...
Instability of Abyssal Currents in a Continuously Stratified Ocean with Bottom Topography
Abyssal Currents Continuously Stratified Ocean Bottom Topography
2008/6/25
A theory is developed for the baroclinic destabilization of density-driven abyssal flows over topography in a rotating environment. The dominant instability mechanism being studied is the release of a...