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hklion authored Jan 30, 2025
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The Regional Model of the Ocean Refined Adaptively (REMORA) is a new implementation
of an existing community standard ocean model,
the Regional Ocean Modeling System
[ROMS, @shchepetkin.mcwilliams:05; @haidvogel.ea:08] that simulates estuarine and oceanic
[ROMS, @haidvogel.ea:08; @shchepetkin.mcwilliams:05] that simulates estuarine and oceanic
dynamics using the latest high-performance computing architectures.
REMORA employs hierarchical parallelism using an MPI+X model, where X may be OpenMP on
multicore CPU-only systems, or CUDA, HIP, or SYCL on GPU-accelerated systems.
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Like ROMS, REMORA:

- solves the incompressible time-dependent Navier-Stokes equation with the Boussinesq and hydrostatic approximations [see @shchepetkin.mcwilliams:05; @haidvogel.ea:08].
- solves the incompressible time-dependent Navier-Stokes equation with the Boussinesq and hydrostatic approximations [@haidvogel.ea:08; @shchepetkin.mcwilliams:05].
- uses a curvilinear Arakawa C-grid.
- uses a stretched, terrain-following vertical s-coordinate.
- uses a split-explicit time-stepping scheme, where several fast barotropic (2D) steps take place within each baroclinic (3D) update [see @shchepetkin.mcwilliams:05].
- uses a split-explicit time-stepping scheme, where several fast barotropic (2D) steps take place within each baroclinic (3D) update [@shchepetkin.mcwilliams:05].
- advances baroclinic steps with a third-order Adams-Bashforth scheme.
- advances barotropic steps with a leapfrog predictor followed by a three-time Adams-Moulton corrector.
- advances scalars with a leapfrog step with a trapezoidal correction.
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