DYAMOND Summer low-resolution simulation
#3458
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artifacts/artifact_funcs.jl
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We want to drop support for this older artifact getter file/functions (any such retrieval function will now be defined within the AtmosArtifacts utility module, making use of the clima_artifact macro ; so the DYAMOND_SUMMER_ICS_p98dev_dataset_path() function is not necessary.
| @@ -7,6 +7,7 @@ function trigger_download(lazy_download = true) | |||
| @info "topo dataset path:`$(topo_res_path())`" | |||
| @info "MiMA convective gravity wave path:`$(mima_gwf_path())`" | |||
| @info "GFDL OGWD test data:`$(gfdl_ogw_data_path())`" | |||
| @info "DYAMOND summer initial conditions path:`$(DYAMOND_SUMMER_ICS_p98deg_dataset_path())`" | |||
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Same as the artifact_funcs.jl file - everything moving forward is expected to rely on the AtmosArtifacts utility module; so this change is not required.
- use "Earth" topography - reduce dt to 1 sec and add some diagnostics for debugging purposes
sriharshakandala
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DYAMOND Summer low-resolution simulation
| Y.f.u₃ .= | ||
| ᶠinterp.( | ||
| ClimaCore.Geometry.Covariant3Vector.( | ||
| ClimaCore.Geometry.WVector.(vel) | ||
| ) | ||
| ) |
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I found that it helps with stability if u₃ is not prescribed.
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This seems to be consistent with @akshaysridhar 's earlier observations !
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I think it’s because the initial w is too large for our timestep. We can consider adding a threshold too.
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DYAMOND Summerlow-resolution simulation.To-do
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