Hello all,
I'm running a 36-year WRF simulation with 6-hourly met_em output, which generates ~5-6 TB of intermediate files. This raises a storage question:
Why do met_em files contain interior grid points for all timesteps when they're only needed for the initial condition (T=0)?
After the first time step, WRF only needs lateral boundary conditions, yet every met_em file contains the full 3D domain. For long climate simulations, this creates massive storage overhead.
Questions:
I understand real.exe needs complete fields for vertical interpolation and consistency checks, but it seems inefficient to store full domains for what becomes pure boundary forcing.
Any insights or workarounds would be appreciated!
Best,
I'm running a 36-year WRF simulation with 6-hourly met_em output, which generates ~5-6 TB of intermediate files. This raises a storage question:
Why do met_em files contain interior grid points for all timesteps when they're only needed for the initial condition (T=0)?
After the first time step, WRF only needs lateral boundary conditions, yet every met_em file contains the full 3D domain. For long climate simulations, this creates massive storage overhead.
Questions:
- Is there a way to generate met_em files with only boundary points after T=0?
- Or can ungrib/metgrid be configured to skip interior points for t>0?
- Has anyone implemented a workflow to delete interior data from met_em files before running real.exe?
I understand real.exe needs complete fields for vertical interpolation and consistency checks, but it seems inefficient to store full domains for what becomes pure boundary forcing.
Any insights or workarounds would be appreciated!
Best,