Titlebook: Nonlinear Processes in Geophysical Fluid Dynamics; A tribute to the sci O. U. Velasco Fuentes,J. Sheinbaum,J. Ochoa Book 2003 Springer Scie

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书目名称Nonlinear Processes in Geophysical Fluid Dynamics影响因子(影响力)




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书目名称Nonlinear Processes in Geophysical Fluid Dynamics网络公开度学科排名




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书目名称Nonlinear Processes in Geophysical Fluid Dynamics被引频次学科排名




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书目名称Nonlinear Processes in Geophysical Fluid Dynamics年度引用学科排名




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书目名称Nonlinear Processes in Geophysical Fluid Dynamics读者反馈学科排名

cortex

Deep Ocean Influence on Upper Ocean Baroclinic Instability Saturation,thin the upper layer (above the thermocline). We confront quasigeostrophic baroclinic instability properties of a 2.5-layer model with those of a 3-layer model with a very thick deep layer, which has been shown to predict spectral instability for basic state parameters for which the 2.5-layer model

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Constrained-Hamiltonian Shallow-Water Dynamics on the Sphere,e velocity field to the height field in Hamilton’s principle for rotating shallow-water dynamics, constitutes an important prototype of Hamiltonian balanced models. Instead of Salmon’s original approach, which consists in taking variations of particle paths at fixed Lagrangian labels and time, Holm’

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Hamiltonian Description of Fluid and Plasma Systems with Continuous Spectra,ed for ascertaining stability in Hamiltonian fluid and plasma systems is only the first step. A complete description involves changing to coordinates in which the energy is diagonal. This amounts to a transformation to action-angle variables. Because fluid and plasma systems typically have a continu

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ENACT

Nonlinear Outflows on a , Plane,tation of the boundary along which they are situated. Both outflows associated with eastern and southern boundaries split into two branches. One branch contains a chain of eddies and the other corresponds to a steady boundary current. Outflows situated along a western boundary, on the other hand, pr

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Mean and Eddy Dynamics of the Main Thermocline,abit it. In classical theories, that is theories that assume a steady, near-laminar flow and that are based on the planetary geostrophic equations, the upper thermocline (below the surface mixed layer) is conservative and advectively dominated — that is, the dominant balance in the thermodynamic equ

NEXUS

An Overview of the Physical Oceanography of the Gulf of California,e most important being strong tidal mixing, some of it close to deep stratification. Three-dimensional numerical model results suggest that tidal mixing may be more important than the thermohaline circulation in causing the long-term residual circulation, which consists of outflow in the upper 200 m