Hi Jorrit,
My starting point would be the expression for Secchi depth that is being used, to see if that could be modified to depend only on attenuation, not on irradiance (e.g., I know of formulations that depend only on the vertical attenuation coefficient of diffuse downwelling irradiance). That would allow Secchi depth to be properly defined at night too. Should that fail, it would be an option to give the Secchi depth a dedicated “missing value” when it is not defined, instead of zero, and to make the temporal averaging scheme exclude such missing values. But that’s more involved.
In any case, the trouble is that I’m not familiar with that "v5.2.2-au" branch of GOTM. It does not seem to be in official repository at https://github.com/gotm-model/code. Without seeing the code, it is difficult to comment further.
Cheers,
Jorn
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Hi Jorrit,
Here’s some info:
https://doi.org/10.1016/j.rse.2007.06.009
https://ereefs.aims.gov.au/ereefs-aims/gbr4/bgc/hindcast/secchi_kd-490_epipar-sg
Ultimately, they use an inverse relationship between Secchi depth and attenuation, which seems to come from this 1929(!) paper: https://doi.org/10.1017/S0025315400029829.
However, these studies describe the link between near-surface attenuation and Secchi depth. Since attenuation is potentially depth-dependent in GOTM (if using feedbacks from biogeochemistry), you may want to somehow consider its vertical variation, e.g., by finding the depth where the remaining radiation is some fraction (e.g., exp[-1.7]=0.18 according to Poole & Atkins) of the surface downwelling value. That could still be done without needing the actual radiation, and therefore should work at night.
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