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Jeroen strongly advises against extrapolating tracers and velocities all the way to the bottom before interpolation. Instead, he recommends to do horizontal interpolation (or diffusion). His recommend…
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Create a new documented example to decompose temperature (or other scalar) anomalies into isopycnal heaving (HVE) and changes along isopycnals (WMP)
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Currently the slope triad computations (the critical ingredient of the redi parameterization) are defined to do horizontal gradients in model index space, see here
https://github.com/E3SM-Project/E…
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Hello,
I recently started computing the Surface Water-Mass Transformation and I found a more efficient and quicker way to do the binning in density space. It requires `flox` a library that allows …
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Suggestion from J. Toole: perhaps we should write cost functions to constrain 1) isopycnal depth and 2) the salinity - or temperature - on isopycnals?
"The variance of Theta/S - below the surfa…
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@zyaj is there an example case that uses isopycnal coordinate and has open boundaries? The iwave_** test cases all seem to be for an initial value problem. Cheers
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MPAS-O cannot currently run in 2-layer mode, e.g.,
```fortran
Doing timestep 0001-01-01_00:10:00
Computing surface flux arrays
Computing forward time step
At line 254 of file mpas_ocn_…
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Eventually, 3D grids should come with methods for projecting 3D fields onto 2D isosurfaces (ex : temperature on an isopycnal).
This issue gathers informations / ideas as to how to proceed.
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The 'convective adjustment' performed prior to building the continuous isopycnal coordinate only rearranges layer thicknesses, temperatures, and salinities. If a water column is statically unstable, t…
ashao updated
4 years ago
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If we are interested in changing the Redi diffusion coefficient. Which variable would that be?
In data.gmredi I find:
GM_isopycK: isopycnal diffusion coefficient (default=GM_background_K)
GM_bac…