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Dynamical Oceanography. Part I: Fundamental Principles
Robert O. Reid
Contents
Kinematics of Fluids
Scalars, vectors and tensors
Vector and indicial notation
Gradient of a scalar field
Divergence of a vector field
Curl of a vector field
The Lagrangian and Eulerian descriptions of motion
Methods of representation of a vector field
Acceleration: Lagrangian description
Acceleration: Eulerian description
The basic kinematic modes of a fluid
Vorticity
Circulation
Stokes' theorem
Vorticity in polar coordinates
Computation of vorticity and circulation
Deformation
Divergence
Deformation in two dimensions
Kinematic classification of fluid motion
Streamfunction for two-dimensional flow
Velocity potential
Laplacian flow
Conformal mapping
Kinematic boundary condition
Application of the boundary condition for Laplacian flow adjacent to a solid cylinder
Kelvin's theorem of minimum kinetic energy
Addition of velocity potentials
Geostatics and Dynamics: The Earth as a Reference System
Absolute gravitational force
Gravity
Gravity anomalies
Tidal forces
Equilibrium of the earth-moon system
Tidal forces associated with the moon
Tidal forces associated with the sun
The equlibrium surface or tide potential
The time variation of the tidal forces
Conservative force field
Geopotential
Configuration of level surfaces on the Earth
The sea level reference geoid
Changes in the reference geoid associated with variations in the angular speed of the earth
Geometrical spacing of the equigeopotential surfaces in the sea and the air
Dynamic height and dynamic depth
Relative velocity in a moving coordinate system
Rate of change of a vector in a moving coordinate system
Relative and absolute acceleration
Geostrophic acceleration
Other accelerations related to the earth's motion
Fluid Density and Hydrostatic Pressure
A fluid defined
A fluid mixture
Isotropy of hydrostatic pressure
Fluid density defined
The hydrostatic equation
Units of pressure
Quasi-hydrostatic conditions
Homogeneous fluid
Barotropic fluid
Baroclinic fluid
The two-layer model
Slopes of the isobaric surfaces in a two-layer barotropic fluid
Relation between isobaric slopes and isopycnal slopes in a baroclinic fluid
The equation of state for sea water
Isobaric slopes in terms of the field of temperature and salinity
Potential density and sigma-t
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
Some Special Laws of Non-Advective Transfer of Properties
Fourier's law of heat conduction
Diffusion
Viscous stresses
Diffusion-drag theory
References
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Steve Baum
Mon Dec 1 08:50:29 CST 1997