A Semi-Implicit Free Surface Formulation for the Semi-Collocated Grid Diecast Ocean Model

Abstract

Under funding from the Office of Naval Research (ONR), the Mississippi State University Center for Air Sea Technology (CAST) presents a semi-implicit free-surface formulation for the DieCAST Ocean model that retains the accurate, low dissipation numerics of its latest and best semi collocated rigid lid version. The approach involves integrating the time implicit (trapezoidal) shallow water equations on a staggered Arakawa 'c' grid, with vertically averaged baroclinic forcing terms determined on a non-staggered Arakawa 'a' grid, including a fourth-order-accurate baroclinic pressure gradient. The shallow water equation numerics are virtually equivalent to standard sigma coordinate approaches for the model barotropic mode. In application to transient wind forced lake Kelvin waves, the new free-surface version gives virtually identical results to the corresponding strongly validated rigid lid DieCAST version (reflecting the fact that the rigid lid barotropic mode numerics are also a sigma-like approach,) and requires less than 50 percent more computing. Thus, the numerics used by both rigid lid and free-surface DieCAST versions combines the best of z-level and sigma coordinate numerics, as well as, the best of 'a' and 'c' grid numerics.

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Document Details

Document Type
Technical Report
Publication Date
Apr 15, 1998
Accession Number
ADA343216

Entities

People

  • Avichal Mehra
  • David E. Dietrich

Organizations

  • Mississippi State University

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Australia
  • Computational Fluid Dynamics
  • Equations
  • Fluid Dynamics
  • Frequency
  • Geography
  • Great Lakes
  • Military Research
  • Mississippi
  • Oceanography
  • Pressure Gradients
  • Shallow Water
  • Standards
  • Surface Waves
  • Three Dimensional
  • Topography
  • Universities

Readers

  • Finite Element Method (FEM) for solving Partial Differential Equations (PDEs)
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers