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Description
At some point in the history of CABLE development the allocation of downwelling shortwave radiation into direct and diffuse components has gained bug for offline studies - this likely occurred at the time when the code considered the fractionation between visible and near-infrared radiation.
The direct-diffuse radiation (unless provided via other means) is evaluated through the use of the spitter function. Originally this assigned the fractions based on the ratio of the timestep's shortwave radiation to a clear sky value (at that location and time of year). When the partitioning between VIS:NIR occurred spitter was not adjusted and currently the call takes in the current VIS (or NIR) shortwave and compares to the clear sky value for total shortwave radiation (not the clear sky value for the VIS (or NIR) shortwave). The ratio evaluated is then smaller than expected - and the diffuse fraction diagnosed is greater than it would be.
If only for testing purposes - we need to retrofit the model to allow for the original intent of spitter to be used.
This implementation will need to be different in the current MAIN (CABLE3) and in the CABLE-POP-TRENDY/NESP2pt9/BLAZE branches because of the code structure.
see also #355