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                       Regional Ocean Modeling System (ROMS)
   ROMS framework diagram illustrates various computational pathways: standalone or coupled to atmospheric and/or wave models. It follows the Earth System Modeling Framework (ESMF) conventions for model coupling: initialize, run and finalize. The dynamical kernel of ROMS is comprised of four separate models including the nonlinear (NLM), tangent linear (TLM), representer tangent linear (RPM), and adjoint (ADM). There are several drivers to run each model (NLM, TLM, RPM, and ADM) separately and together.
   ROMS is a free-surface, terrain-following, primitive equations ocean model widely used by the scientific community for a diverse range of applications (e.g., Haidvogel et al., 2000;...; Warner et al., 2005a,b; Wilkin et al., 2005).
   The algorithms that comprise ROMS computational nonlinear kernel are described in detail in Shchepetkin and McWilliams (2003, 2005), and the tangent linear and adjoint kernels and platforms are described in Moore et al. (2004).
   ROMS includes accurate and efficient physical and numerical algorithms and several coupled models for biogeochemical, bio-optical, sediment, and sea ice applications. The sea ice model is described in Budgell (2005).
   It also includes several vertical mixing schemes (Warner et al., 2005a), multiple levels of nesting and composed grids.
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