Abstract
A two-time-level, three-dimensional numerical ocean circulation model is established with a two-level, single-step Eulerian time-difference scheme. The mathematical model of the large-scale oceanic motions is based on the terrain-following coordinated, Boussinesq, Reynolds-averaged primitive equations of ocean dynamics. A simple but very practical Eulerian forward-backward method is adopted to replace the most preferred leapfrog scheme as the time-difference method for both barotropic and baroclinic modes. The forward-backward method is of the second order of accuracy, requires only once of the function evaluation per time step, and is free of the computational mode inherent in the three-level schemes. It is superior in many respects to the original leapfrog and Asselin-filtered leapfrog schemes in the practical use. The performance of the newly-built circulation model is tested by simulating a barotropic (tides in marginal seas of China) and a baroclinic phenomenon (seasonal evolution of the Yellow Sea Cold Water Mass), respectively. The three-year time histories of four prognostic variables obtained by the POM model and the two-time-level model are compared in a regional simulation experiment for the northwest Pacific to further show the reliability of the two-level scheme circulation model.
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Project supported by the National Science Foundation of China (Grant No. 40906017, 41376038), the National High Technology Research and Development Program of China (863 Program, Grant No. 2013AA09A506).
Biography: HAN Lei (1981-), Male, Ph. D. Senior Engineer
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Han, L., Yuan, Yl. An ocean circulation model based on Eulerian forward-backward difference scheme and three-dimensional, primitive equations and its application in regional simulations. J Hydrodyn 26, 37–49 (2014). https://doi.org/10.1016/S1001-6058(14)60005-6
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DOI: https://doi.org/10.1016/S1001-6058(14)60005-6