Open AccessA nonhydrostatic version of FVCOM: 1. Validation experiments
Author(s) -
Lai Zhigang,
Chen Changsheng,
Cowles Geoffrey W.,
Beardsley Robert C.
Publication year - 2010
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2009jc005525
Subject(s) - finite volume method , baroclinity , unstructured grid , grid , mechanics , flow (mathematics) , volume (thermodynamics) , geology , meteorology , computer science , physics , geodesy , quantum mechanics
The unstructured grid finite volume coastal ocean model (FVCOM) system has been expanded to include nonhydrostatic dynamics. This addition uses the factional step method with both split mode explicit and semi‐implicit schemes. The unstructured grid finite volume method, combined with a correction of the final free surface from its intermediate value with inclusion of nonhydrostatic effects, efficiently reduces numerical damping and thus ensures second‐order accuracy of the solutions with local/global volume conservation. Numerical experiments have been made to fully validate the nonhydrostatic FVCOM, including surface standing and solitary waves in idealized flat‐ and sloping‐bottomed channels in homogeneous conditions, the density adjustment problem for lock exchange flow in a flat‐bottomed channel, and two‐layer internal solitary wave breaking on a sloping shelf. The model results agree well with the relevant analytical solutions and laboratory data. These validation experiments demonstrate that the nonhydrostatic FVCOM is capable of resolving complex nonhydrostatic dynamics in coastal and estuarine regions.