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@daveweisberg Can you point a baseline case obtained with GASC with divertor heat flux constraints?
e.g. q parallel upstream, q_parallel_target and impurities fractions
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(1) Outgoing radiation assuming no aerosol
rlutaf, rlutcsaf, rsutaf: need a standard names. Current names do not include aerosol free component.
- rlut, rlutaf: toa_outgoing_longwave_flux
- rlutc…
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Unlike #39, here, we change the surface heat fluxes on the globe by a certain factor. The idea is to add heat to subtropics and lose out heat from the subpolar regions. So, in a way, not only are we c…
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We have successfully created a set of simulations where changing one doesn't affect the other. In the following issue, we discuss a set of experiments where we change the heat flux everywhere by a cer…
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During the development of the 0.25° ocean used in CM4, explicit land model heat fluxes from rivers and calving were not used. Instead, the heat fluxes on the ocean side assume a temperature equal to …
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When we use specific heat capacities with a TEOS-10 equation of state we should use the value from equation (3.3.3) of the TEOS-10 manual.
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Hi, my model has radiative heat flux gauges but the checker is not recognising them. I believe it might be because my devices are referred to as "radiative heat flux gas" when the checker might just b…
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# Challenge 15 - Benchmarking surface heat fluxes
> **Stream 1** - Software Development for Earth Sciences
### Goal
Adapt existing software package to include a meaningful benchmarking stra…
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I think these are defined at faces (double check with J. Lore), so we'll need #6 to fully support this work.
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Can we replace the for loop in cell 8 here:
https://cosima-recipes.readthedocs.io/en/latest/DocumentedExamples/Meridional_heat_transport.html#Method-2:-using-from-the-net-surface-heat-flux-(assumin…