Estuarine and Wetland Processes 1980
DOI: 10.1007/978-1-4757-5177-2_6
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Evolution of a Numerical Model for Simulating Long-Period Wave Behavior in Ocean-Estuarine Systems

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Cited by 20 publications
(14 citation statements)
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“…The simplest of horizontal coordinate transformations are those that stretch coordinates to form a numerical grid that is rectangular but not uniform. The transformation used by Butler (1978Butler ( , 1980, and also implemented in the 3-D model by Sheng (1983) Noye and Stevens (1987) used the same horizontal transformation as Boericke and Hall but solved the transformed governing equations by using a nonuniform grid spacing in order to increase the grid resolution in regions of interest within the original coordinate system. The nonuniform grid spacing in the computational space must be chosen according to certain criteria presented by Noye and Stevens to retain the accuracy of the numerical approximations that are achievable for uniformly spaced grids.…”
Section: Horizontal Coordinate Transformationsmentioning
confidence: 99%
“…The simplest of horizontal coordinate transformations are those that stretch coordinates to form a numerical grid that is rectangular but not uniform. The transformation used by Butler (1978Butler ( , 1980, and also implemented in the 3-D model by Sheng (1983) Noye and Stevens (1987) used the same horizontal transformation as Boericke and Hall but solved the transformed governing equations by using a nonuniform grid spacing in order to increase the grid resolution in regions of interest within the original coordinate system. The nonuniform grid spacing in the computational space must be chosen according to certain criteria presented by Noye and Stevens to retain the accuracy of the numerical approximations that are achievable for uniformly spaced grids.…”
Section: Horizontal Coordinate Transformationsmentioning
confidence: 99%
“…Approaches to examine plan impacts include modeling, and in the cases of Los Angeles and Long Beach Harbors, there have been several numerical model studies of tidal circulation (Chiang and Lee 1982, Seabergh andOutlaw 1984, Seabergh 1985). Most of the previous numerical circulation studies were performed using depth-averaged models such as WIFM (Butler 1980) and using only tides for forcing. Recently, the ports, together with the U.S. Army Engineer District, Los Angeles and the U.S. Army Engineer Waterways Experiment Station (WES), embarked on a Harbors Model Enhancement (HME) Program.…”
Section: Contentsmentioning
confidence: 99%
“…Models currently being used at the Waterways Experiment Station (WES) include the finite difference model WIFM (WES Implicit Flooding Model), which evolved from early work by Leendertse (1967Leendertse ( , 1973. The model and its application have been refined and significantly improved at WES, and have been described at different stages of development by Butler (1980) . The finite element flow model of Research Management Associates (RMA-2V) (Ariathurai and Arulanadan 1978) evolved rom work by Norton et al (1973) sponsored by US Army Engineer District, Walla Walla.…”
Section: Bmentioning
confidence: 99%