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Maps from the Mid-Ocean Dynamics Experiment：Part II. Potential vorticity and its Conservation
Mid-Ocean Dynamics Experiment Conservation Potential vorticity
2009/3/7
Observations of float trajectories and vertical density profiles from the Mid-Ocean Dynamics Experiment are analyzed in terms of a likely equation of motion for mesoscale eddies involving the conserva...
Conservation Calculations in Natural Coordinates (with an Example from the Baltic)
Conservation Calculations Natural Coordinates
2009/2/13
Conservation expressions for a fluid property i* (e.g., salt, heat) and mass are derived for a semi-enclosed, stratified region as functions of a concentration j (e.g., salinity, temperature) and time...
Quasi-linear Eddy-Viscosity Model for the Flux of Energy and Momentum to Wind Waves Using Conservation-Law Equations in a Curvilinear Coordinate System
Curvilinear Coordinate System Quasi-linear Eddy-Viscosity Model
2008/12/22
The airflow above ocean waves is calculated using a quasi-linear model—one in which the effect of the waves on the mean flow is taken into account. The model uses curvilinear coordinates, in which one...
The Temporal-Residual-Mean Velocity. Part I：Derivation and the Scalar Conservation Equations
temporal-residual-mean Scalar Conservation Equations eddy fluxes
2008/12/11
The time-averaged density conservation equation in z coordinates contains a forcing term that is the divergence of the transient eddy fluxes. These fluxes are due to the temporal correlation between t...
On Conservation Equations in Oceanography: How Accurate Are Boussinesq Ocean Models
Conservation Equations Oceanography Boussinesq Ocean Models
2008/6/6
Traditionally, the conservation equations in oceanography include the Boussinesq approximation, and the velocity variable is interpreted as the Eulerian mean velocity averaged over turbulent scales. I...