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Merge pull request #318 from hklion/docs
add readmes to problems and tweak docs
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.. include:: building.rst | ||
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.. include:: InputFiles.rst | ||
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.. include:: testing.rst |
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The Advection problem tests scalar advection of a gaussian concentration | ||
distribution on a doubly-periodic domain with flat bathymetry. | ||
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The file called inputs contains the single-level version of this test. The | ||
file called inputs_ml runs the problem with adaptive mesh refinement, refining | ||
where the scalar has a value greater than 0.5. |
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This problem reproduces the reentrant channel test case from []. It tests | ||
the development of turbulence and the GLS mixing scheme. The mean surface | ||
kinetic energy agrees with that from ROMS. |
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The DoubleGyre problem reproduces the classic wind-driven double gyre problem, | ||
similar to the ROMS test problem by the same name. |
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The basic version of the DoublyPerioidic test simulates a flow with a | ||
depth-dependent horizontal velocity and temperature profile in a | ||
doubly-periodic domain with flat bathymetry. When non-flat bathymetry | ||
is used, the depth profile is the same as in the ROMS (and REMORA) | ||
Upwelling problem. | ||
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This small idealized grid is used to test netCDF-provided initial and boundary | ||
conditions. The ocean is initialized with zero velocity and a constant | ||
temperature and salinity. Time-varying boundary conditions are then applied | ||
for velocity, temperature, or salinity (provided by netCDF file). The default | ||
is to used a clamped boundary condition for all quantities, but options for | ||
Chapman-Flather and radiation conditions are available. This test also | ||
verifies correct behavior with land-sea masking when using the ``_masked`` grid | ||
file. | ||
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The netCDF files needed to run these tests can be found in the | ||
`remora-data <https://github.com/seahorce-scidac/remora-data>`_ | ||
repository under the ``IdealMiniGrid`` directory. | ||
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This problem tests advection of tracer particles on a flat domain. |
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The Seamount problem is a standard test in | ||
`ROMS <https://www.myroms.org/wiki/SEAMOUNT_CASE>`_. | ||
The problem involves an (analytically) stably stratified fluid at rest over a | ||
seamount. In the absence of numerical errors, the fluid will remain at rest. | ||
However, this may not occur due to numerical errors in the calculation of the | ||
horizontal pressure gradient when the vertical coordinates are misaligned with | ||
the geopotential surfaces, as is the case in problems with spatially-varying | ||
bathymetry in ROMS/REMORA. | ||
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The Upwelling problem is set up as in | ||
`ROMS <https://www.myroms.org/wiki/UPWELLING_CASE>`_. It demonstrates | ||
wind-driven upwelling over a perioidc channel. |