|Radiative forcings at top of the atmosphere (TOA) (def. positive down)
|Note: Forcing definitions based on Ghan (2013) for SW have been extended to apply also for LW fluxes.
Note that all LW fluxes are positive downwards, opposite of the SW fluxes, so that the sum of SW & LW
should be (and is for
"SW + LW") calculated as SW - LW.
NOTE 2: When the model is run with MACv2-SP aerosols (with define SPAER), the figures on this page
make no sense and should therefore not be used. This is the case for the experiment shown to the right.