Here, z is the elevation above the bed, c _ s is the concentration of suspended sediment at that elevation, h is the flow depth, P is the Rouse number, and \ alpha relates the eddy viscosity for momentum K _ m to the eddy diffusivity for sediment, which is approximately equal to one.
12.
In 1948 Henry Stommel proposed a circulation for the entire ocean depth by starting with the same equations as Sverdrup but adding bottom friction, and showed that the variation in Rossby ( eddy viscosity ), Sverdrup ( upper ocean wind driven flow ) and Stommel ( western boundary current flow ) and proposed a complete solution for the ocean circulation.
13.
By the adoption of the eddy viscosity concept these effects are expressed through the eddy viscosity, which is optionally determined by one of the following five closure models : a constant eddy viscosity; the Smagorinsky sub-grid ( zero-equation ) model; the k-( one-equation ) model; the standard k-? ( two-equation ) model; and a combination of the Smagorinsky model for the horizontal direction and a k-? model for the vertical direction.
14.
By the adoption of the eddy viscosity concept these effects are expressed through the eddy viscosity, which is optionally determined by one of the following five closure models : a constant eddy viscosity; the Smagorinsky sub-grid ( zero-equation ) model; the k-( one-equation ) model; the standard k-? ( two-equation ) model; and a combination of the Smagorinsky model for the horizontal direction and a k-? model for the vertical direction.
15.
By the adoption of the eddy viscosity concept these effects are expressed through the eddy viscosity, which is optionally determined by one of the following five closure models : a constant eddy viscosity; the Smagorinsky sub-grid ( zero-equation ) model; the k-( one-equation ) model; the standard k-? ( two-equation ) model; and a combination of the Smagorinsky model for the horizontal direction and a k-? model for the vertical direction.
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