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Goodman, Louis - School for Marine Science and Technology, University of Massachusetts, Dartmouth
Acoustic scattering from a thermally driven buoyant plume revisited John Oeschger
What is turbulence? Why is it important in the Ocean?
Math Review We are already familiar with the concept of a scalar and vector.
Momentum Equations in a Fluid density of water
Problem Set # 2 1. Given an incompressible 2D flow with "x'" and "z" velocity given by
Problem Set # 3 1. Why do we use 10U the wind speed 10 m above the surface, in the drag formula
Problem Set # 4 1. Using the complex solution exp[ (1 ) ]
Mixing and Turbulent Diffusion in the Ocean Trace Metals
Problem Set # 6 1. An factory smoke stack releases intense small spherical patch of dust particles of
1. For the generic turbulence model assuming 2 1 (a) show that
Turbulence in Coastal Fronts near the Mouths of Block Island and Long Island Sounds
Laminar Flow Turbulent Flow
RESUME: Louis Goodman ADDRESS: 161 Narragansett Blvd Telephone: (H) 401 293 0766
Concept of Reynolds Number, Re Acceleration Advection Pressure Gradient Friction
MAR610/MNE490 Problem Set #1 1. (a) Show that ijkijk = 6
Time or Space ' Fluctuating
Horizontal Equation of Motion v ( ) ( )i i i i i i i
On Measuring the Terms of the Turbulent Kinetic Energy Budget from an AUV LOUIS GOODMAN
Turbulent dissipation in a near-field river plume: A comparison of control volume and microstructure observations with
On the theory of advective effects on biological dynamics in the sea. III. The role of
Problem Set # 5 1. In a stratified flow the energy containing eddies have a time scale of N-1
Please cite this article in press as: Goodman, L., Application of the Robinson biodynamical theory to turbulence. Dyn. Atmos. Oceans (2011), doi:10.1016/j.dynatmoce.2011.05.003
On observing acoustic backscattering from salinity turbulence Louis Goodman4
Submesoscale Spatial Variability of Ocean Turbulence L GoodmanL. Goodman