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The Four Basic Principles
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Dynamical Oceanography. Part I:
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Hydrostatic stability
The Fundamental Equations of Hydro-Thermo-Dynamics of a Real Fluid
The Four Basic Principles
Fluid Velocity
The Equation of Continuity
The Continuity of Salt
Advective and Non-Advective Transport
Non-Conservative Constituents
Conservation of Momentum: The Equations of Absolute Motion
Symmetry of the viscous stress tensor
Equation of relative motion on the rotating earth
Generation and dissipation of mechanical energy
Conservation of total energy
The first law of thermodynamics
A special case of the first law
Temperature and entropy-the Kelvin hypothesis
A more general form of the Kelvin hypothesis for pure fluids
Gibbs' extension of the Kelvin hypothesis to fluid mixtures
Evaluation of the equations of state for gases
Some further consequences of the Kelvin hypothesis
The second law of thermodynamics
The integral form of the second law
Extension of equations for mixtures to more than two constitutents
Free energy function
Mixture of ideal gases
Some direct consequences of the second law in regard to the behavior of the entropy function
Boundary conditions for the flux of salt and the kinematic condition in the presence of evaporation
Boundary condition on the temperature or heat flux at the surface
Boundary condition on the stress
Summary of fundamental relations
Next:
The Four Basic Principles
Up:
Dynamical Oceanography. Part I:
Previous:
Hydrostatic stability
Steve Baum
Mon Dec 1 08:50:29 CST 1997