@@ -170,7 +174,7 @@ Not yet there, but getting close...... Namelist parameters and input forcing fil
**Modifications to linking input files**
While many input forcing files need to change, this is done by changing the link/pointing. However, to run with slab ocean, you'll need an extra file, the `heatflux` or `qflx` file. This is normally obtained by running a pure aquaplanet run first, and post-processing the output to get a climatological (maybe also zonally symmetric) flux file, that is then used as an input to the slab ocean part. Assume for the moment you have this file `T63_heatflux_test.nc`. There are also two other files that are not necessarily readily available, `T63GR15_surf_aqua_irad_noseason_final.nc` and `T63_ozone_historical_1850.nc`\
While many input forcing files need to change, this is done by changing the link/pointing. However, to run with slab ocean, you'll need an extra file, the `heatflux` or `qflx` file. Assume for the moment you have this file `T63_heatflux_test.nc`. There are also two other files that are not necessarily readily available, `T63GR15_surf_aqua_irad_noseason_final.nc` and `T63_ozone_historical_1850.nc`\
Below, unless otherwise stated, `#` means to comment these lines out and be sure to add the new pointers.
1. 3d initial file of atmosphere (spectral, no dependence on lsmask)
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@@ -249,6 +253,12 @@ Below, unless otherwise stated, `#` means to comment these lines out and be sure
A little more on preparations of these input files, particularly for aquaplanet slab ocean.
- The 'qlfx' file is normally obtained by first running a slab ocean aquaplanet with zero flux correction in order to get the climatological SST. The SST is then used to run a pure aquaplanet run with prescribed SST so that we can then compute the surface flux. This surface flux then requires post-processing to get a climatological (12 months) zonally invariant and hemispherically symmetric flux file, that is then used as an input to the slab ocean part.
- Ozone file needs a vertical profile to ensure radiative properties of the stratosphere and troposphere, but for an aquaplanet slab ocean, we would need zonally invariant and hemispherically symmetric ozone concentrations.
- Solar irradiance must have no seasons. Here, we ensure eccentricity and obliquity is also set to zero. However, all these do not account for varying zenith angle of the sun.