@@ -170,7 +174,7 @@ Not yet there, but getting close...... Namelist parameters and input forcing fil
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@@ -170,7 +174,7 @@ Not yet there, but getting close...... Namelist parameters and input forcing fil
**Modifications to linking input files**
**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.
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)
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
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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.