# Discretization

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The original version of FVCOM was developed in the σ-coordinate transformation system. The code was subsequently upgraded to the generalized terrain-following coordinate system in 2006. The discretization forms of governing equations have been significantly modified in this new coordinate system. When the non-hydrostatic version of FVCOM was developed, we implemented a semi-implicit solver, so the current version of FVCOM has two options for the time integration: 1) mode-split and 2) semi-implicit. In this chapter, we provide an example of the discrete forms of the hydrostatic FVCOM in the σ-coordinate transformation system for the mode-split solver. The σ-coordinate transformation is one selection of the generalized terrain-following coordinates, so learning the details of the discretization forms in this coordinate system can make users it easy to learn how the generalized terrain-following coordinates work in FVCOM. A brief description of the semi-implicit solver is given in Chapter 4 when the non-hydrostatic solver is introduced. Users, who are interested in learning the details of discretization forms in the generalized terrain-following coordinate system, can examine the source code directly. | The original version of FVCOM was developed in the σ-coordinate transformation system. The code was subsequently upgraded to the generalized terrain-following coordinate system in 2006. The discretization forms of governing equations have been significantly modified in this new coordinate system. When the non-hydrostatic version of FVCOM was developed, we implemented a semi-implicit solver, so the current version of FVCOM has two options for the time integration: 1) mode-split and 2) semi-implicit. In this chapter, we provide an example of the discrete forms of the hydrostatic FVCOM in the σ-coordinate transformation system for the mode-split solver. The σ-coordinate transformation is one selection of the generalized terrain-following coordinates, so learning the details of the discretization forms in this coordinate system can make users it easy to learn how the generalized terrain-following coordinates work in FVCOM. A brief description of the semi-implicit solver is given in Chapter 4 when the non-hydrostatic solver is introduced. Users, who are interested in learning the details of discretization forms in the generalized terrain-following coordinate system, can examine the source code directly. | ||

- | == | + | ==Computational Stencil== |

[[Image:FVCOM_horizontal_stencil.png|thumb|100px|right|alt=FVCOM horizontal stencil| FVCOM horizontal stencil]] | [[Image:FVCOM_horizontal_stencil.png|thumb|100px|right|alt=FVCOM horizontal stencil| FVCOM horizontal stencil]] | ||

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To provide a more accurate estimation of the sea-surface elevation, currents and salt and temperature fluxes, ''u'' and ''v'' are placed at centroids and all scalar variables, such as ζ, H, , ω, S, T, ρ, are placed at nodes. Scalar variables at each node are determined by a net flux through the sections linked to centroids and the mid-point of the adjacent sides in the surrounding triangles (called the “tracer control element” or TCE), while u and v at the centroids are calculated based on a net flux through the three sides of that triangle (called the “momentum control element” or MCE). | To provide a more accurate estimation of the sea-surface elevation, currents and salt and temperature fluxes, ''u'' and ''v'' are placed at centroids and all scalar variables, such as ζ, H, , ω, S, T, ρ, are placed at nodes. Scalar variables at each node are determined by a net flux through the sections linked to centroids and the mid-point of the adjacent sides in the surrounding triangles (called the “tracer control element” or TCE), while u and v at the centroids are calculated based on a net flux through the three sides of that triangle (called the “momentum control element” or MCE). | ||

Similar to other finite-difference models such as POM and ROMS, all the model variables except ω (vertical velocity on the sigma-layer surface) and turbulence variables (such as and ) are placed at the mid-level of each σ layer. There are no restrictions on the thickness of the σ-layer, which allows users to use either uniform or non-uniform σ-layers. | Similar to other finite-difference models such as POM and ROMS, all the model variables except ω (vertical velocity on the sigma-layer surface) and turbulence variables (such as and ) are placed at the mid-level of each σ layer. There are no restrictions on the thickness of the σ-layer, which allows users to use either uniform or non-uniform σ-layers. | ||

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+ | ==Discretization in Cartesian Coordinates== | ||

+ | |||

+ | ===2D External Mode=== | ||

+ | |||

+ | <math>\int\int\frac{\partial \zeta}{\partial t} = - \int\int \left[\frac{\partial(\bar{u}D}\partial x} +\frac{\partial(\bar{v}D}\partial y} \right] dx dy | ||

+ | |||

+ | </math> |

## Revision as of 14:28, 14 November 2011

The original version of FVCOM was developed in the σ-coordinate transformation system. The code was subsequently upgraded to the generalized terrain-following coordinate system in 2006. The discretization forms of governing equations have been significantly modified in this new coordinate system. When the non-hydrostatic version of FVCOM was developed, we implemented a semi-implicit solver, so the current version of FVCOM has two options for the time integration: 1) mode-split and 2) semi-implicit. In this chapter, we provide an example of the discrete forms of the hydrostatic FVCOM in the σ-coordinate transformation system for the mode-split solver. The σ-coordinate transformation is one selection of the generalized terrain-following coordinates, so learning the details of the discretization forms in this coordinate system can make users it easy to learn how the generalized terrain-following coordinates work in FVCOM. A brief description of the semi-implicit solver is given in Chapter 4 when the non-hydrostatic solver is introduced. Users, who are interested in learning the details of discretization forms in the generalized terrain-following coordinate system, can examine the source code directly.

## Computational Stencil

Similar to a triangular finite element method, the horizontal numerical computational domain is subdivided into a set of non-overlapping unstructured triangular cells. An unstructured triangle is comprised of three nodes, a centroid, and three sides (Fig. 3.1). Let N and M be the total number of centroids and nodes in the computational domain, respectively, then the locations of centroids can be expressed as:

and the location of the nodes can be specified as:

Since none of the triangles in the grid overlap, *N* should also be the total number of triangles. On each triangular cell, the three nodes are identified using integral numbers defined as where is counted clockwise from 1 to 3. The surrounding triangles that have a common side are counted using integral numbers defined as where is counted clockwise from 1 to 3. At open or coastal solid boundaries, is specified as zero. At each node, the total number of the surrounding triangles with a connection to this node is expressed as *NT(j)*, and they are counted using integral numbers *NB _{i}(m)* where

*m*is counted clockwise from 1 to

*NT(j)*.

To provide a more accurate estimation of the sea-surface elevation, currents and salt and temperature fluxes, *u* and *v* are placed at centroids and all scalar variables, such as ζ, H, , ω, S, T, ρ, are placed at nodes. Scalar variables at each node are determined by a net flux through the sections linked to centroids and the mid-point of the adjacent sides in the surrounding triangles (called the “tracer control element” or TCE), while u and v at the centroids are calculated based on a net flux through the three sides of that triangle (called the “momentum control element” or MCE).
Similar to other finite-difference models such as POM and ROMS, all the model variables except ω (vertical velocity on the sigma-layer surface) and turbulence variables (such as and ) are placed at the mid-level of each σ layer. There are no restrictions on the thickness of the σ-layer, which allows users to use either uniform or non-uniform σ-layers.

## Discretization in Cartesian Coordinates

### 2D External Mode

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