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Something like (needs to be validated):
```python
all_vars = [
"clt", # cloud area fraction
"evspsbl", # evaporation including sublimation and transpiration
"hfls", # surface upw…
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**Martin Juckes**
**13th May 2020**
**`downward_heat_flux_at_snow_base`**
**- Definition**
"Downward" indicates a vector component which is positive when directed downward (negative upward).…
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I get the expected results for Amon from CanESM:
```
$python cfamip.py CanESM5-1_proc/CanESM5-1_r4i1p1f1_Amon_input_files.txt
[,
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,…
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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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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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# The Climate Modeling Alliance
## Software Design Issue 📜
### Purpose
1. Clima ocean has a parameterization that requires that the roughness lengths to be a function of u_star, q_star, \theta_star…
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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.