momentum flux

Study of the heat and momentum fluxes at the air/ocean interface.

However, these are also the units of momentum flux.

Momentum Flux 4 Now, the molecules will collide with one another.

This is the force (or momentum flux) exerted on the water column by the presence of the wave.

In all but the simplest cases the conservation of energy and momentum fluxes is no longer sufficient to determine the flow behaviour.

In addition, momentum flux is one of the parameters to estimate fluid impact on offshore structures.

It is possible for momentum flux to occur even though the wave itself does not have a mean momentum.

The momentum flux tensor has the following form then:

For a square or circle, the momentum fluxes and pressure differences account for half the lift each.

Here, is the momentum flux density and plays a role similar to in Poynting's theorem.

The luminosity-preserving flows can induce pressure gradients that increase the momentum flux with distance.

In this case, the buildup term is inconsequential because all of the field momentum flux is absorbed.

Load and moment boundary conditions involve higher derivatives of and represent momentum flux.

A simple model of the surface layer can be derived by first examining the turbulent momentum flux through a surface.

Eddy momentum flux and its contribution to the Southern Ocean momentum balance.

The boundary layer can be considered to possess a total momentum flux deficit, due to the frictional dissipation.

Distinguishing the influences of heat, freshwater and momentum fluxes on ocean circulation and climate.

Momentum flux, the rate of transfer of momentum across a unit area (N s m s).

First eliminate the pressure "p" from the momentum flux "S" by use of the Bernoulli equation:

The momentum flux "S" then becomes:

Consequently, the momentum flux "S" becomes, again retaining only terms up to proportional to "ζ":

Inner-scale scintillometers can also measure the dissipation rate of turbulent kinetic energy and the momentum flux.

Further analysis may also yield other atmospheric parameters such as scatterer aspect sensitivity, turbulence intensity, tidal components, and momentum fluxes.

Turbulent processes can be roughly combined into three categories: heat flux, moisture flux, and momentum flux.

Beginning with an equal momentum flux M and discharge q upstream and downstream of the hydraulic jump: