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On the Influence of a Lower Layer on the Propagation of Nonlinear Oceanic Eddies
Lower Layer Nonlinear Oceanic Eddies
2008/12/24
The one-layer, reduced-gravity, also called equivalent-barotropic, model has been widely used in countless applications. Although its validity is based on the assumption that a second, lower layer is ...
The Formation of Oceanic Eddies in Symmetric and Asymmetric Jets. Part I：Early Time Evolution and Bulk Eddy Transports
Oceanic Eddies Symmetric Asymmetric Jets Bulk Eddy Transports
2008/12/12
A numerical study of the life cycles of eddies formed in perturbed baroclinic jets, emphasizing the influence of spanwise asymmetry in the initial structure of the jet on the downstream evolution of t...
The Formation of Oceanic Eddies in Symmetric and Asymmetric Jets. Part II：Late Time Evolution and Coherent Vortex Formation
quasigeostrophic Late Time Evolution Coherent Vortex Formation Oceanic Eddies
2008/12/10
The dynamical processes involved in eddy genesis, evolution, and demise as revealed in a series of high-resolution numerical simulations of perturbed oceanic jets are investigated. Comparisons are pro...