This is a summary of the workflow. The details of each tool and the corresponding input data should be read in the corresponding source file.
| binary | inputs | outputs |
|---|---|---|
| inigrid.x | tlab.ini | grid |
| inirand.x | tlab.ini, grid | [flow,scal].rand.? |
| iniflow.x | tlab.ini, grid [,flow.rand.?] | flow.ics.? |
| iniscal.x | tlab.ini, grid [,scal.rand.?] | scal.ics.? |
| binary | inputs | outputs |
|---|---|---|
| dns.x | tlab.ini, grid, flow..?, scal..? | flow..?, scal..? |
| binary | inputs | outputs |
|---|---|---|
| averages.x | tlab.ini, grid, flow..?, scal..? | avg* |
| pdfs.x | tlab.ini, grid, flow..?, scal..? | pdf* |
| spectra.x | tlab.ini, grid, flow..?, scal..? | xsp*, zsp* |
| visuals.x | tlab.ini, grid, flow..?, scal..? | variable files |
- Case01. Shear layer with broadband ICs. Uniform grid. Kelvin-Helmholtz.
- Case02. Same as Case01, but compressible
- Case03. Same as Case01, but with stretched grid.
- Case04. Same as Case03, but compressible.
- Case05. Same as Case03, but 2 scalars with different Schmidt * numbers.
- Case06. Stably stratified density interface with discrete ICs: oscillating inversion.
- Case07. Unstable stratified density interface: Rayleigh-Taylor.
- Case08. Stably stratified shear layer.
-
Case10. Heated plate.
-
Case11. Same as Case09, but two scalars with different BCs.
-
Case12. Convective boundary layer with quadratic chemistry in three passive scalars.
-
Case13. Rayleigh-Benard convection with Dirichlet boundary conditions.
-
Case14. Cloud-top mixing layer, airwater equilibrium compressible formulation.
-
Case15. Cloud-top mixing layer; airwater equilibrium incompressible formulation.
-
Case16. Cloud-top mixing layer; airwaterlinear, evaporation only. (Case06 plus buoyancy reversal.)
-
Case17. Cloud-top mixing layer; airwaterlinear, radiation only.
-
Case18. Cloud-top mixing layer; airwaterlinear, radiation case with evaporative cooling.
-
Case19. Cloud-top mixing layer; airwaterlinear, radiation case with evaporative cooling and settling.
-
Case20. Subsiding shell; airwater. Gravity vector along the horizontal.
-
Case21. Subsiding shell; airwater. Broadband perturbation.
-
Case24. Airwater equilibrium incompressible formulation of stratocumulus-topped boundary layer.
-
Case25. Anelastic formulation of CBL.
-
Case26. Airvapor anelastic formulation of CBL.
-
Case27. Airwater equilibrium anelastic formulation of stratocumulus-topped boundary layer.
-
Case28. Same as Case27, but adding subsidence and sedimentation.
-
Case29. Same as Case28, but with dimensions.
-
Case30. Same as Case29, but with different radiation model.
- Case41. Half Channel flow.
- Case42. Same as 11, implicit solver.
- Case43. Channel flow.
- Case44. Stably stratified channel flow.
- Case46. Wave maker in incompressible case.
- Case51. Case01 (shear layer), saving only the particles.
- Case52. Case01 (shear layer), saving trajectories as well (but fewer particles).
- Case53. Case32, but inertia particles instead of tracers.
- Case54. Case17 (cloud-top), solving liquid equation w/ & w/o diffusion.
- Case55. Same as 34, but with a stratified bottom interface.
- Case70. 1D perturbed laminar Ekman layer, implicit solver.
- Case81. Neutral Ekman layer without sponge at the top.
- Case82. Neutral Ekman layer with sponge at the top.
- Case84. Stable Ekman layer with sponge at the top.
- Case85. Same as 21, implicit solver.
- Case86. Same as 22, implicit solver.
- Case87. Same as 23, implicit solver.
- Case88. Neutral Ekman layer with sponge at the top and interactive BC at the bottom.
- Case91. Channel flow with constant streamwise pressure gradient (Re_tau=180, rotation term for turbulent transition!).
- Case92. Same as 61, with horizontal pressure staggering and a compact vertical pressure filter (without rotation term).
- Case93. Same as 62, with IBM (streamwise aligned bars on lower and upper boundary).