Page 205 - Fundamentals of Ocean Renewable Energy Generating Electricity From The Sea
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194 Fundamentals of Ocean Renewable Energy


            8.1.1 Horizontal Mesh Type
            There is a vast array of ocean models, and a wide range of ways in which they
            can be categorized. There are many places we could begin this classification
            but, because it is of much interest to wave and tidal resource characterization,
            we begin by differentiating between structured and unstructured meshes.
               In a structured grid, all grid lines are orientated regularly so that, in a
            2D case, the coordinate transformations of curvilinear lines result in a square
            (Fig. 8.1A). By contrast, this restriction does not apply to unstructured grids (or
            mesh) (Fig. 8.1B); however, this grid is more complex to deal with numerically.
            The advantage of a structured grid is its simplicity and ease of preprocessing
            and postprocessing; however, to achieve a desired resolution (e.g. to resolve the
            curved geometry shown in Fig. 8.1A), it is necessary to use a constant and high-
            resolution grid throughout the computational domain. Clearly, this resolution is
            easier to achieve by spatially varying the grid resolution, as in an unstructured
            grid (Fig. 8.1B), with the added advantage of lower grid storage (e.g. the circle
            in the centre of Fig. 8.1, which could represent an island, requires no storage
            using an unstructured grid).
               Within the context of ocean energy, it is clear that due to its ability
            to accommodate a wide range of scales within a single-model domain, for
            example, a regional model which incorporates a tidal energy array within a
            narrow strait, unstructured meshes tend to be favoured for resource assessment.
            However, many ocean models, particularly 3D models, which simulate a wide
            range of physical processes, are based on a structured mesh. Under such
            circumstances, a sequence of nested models, with increasing grid resolution
            from outer to inner nests, will be required. In general, structured meshes tend to
            be favoured for larger-scale ocean modelling applications.

























            FIG. 8.1  (A) Structured and (B) unstructured horizontal meshes.
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