ctsm5.4.056: Merge wetlands.n04.ctsm5.4.055 to master - #4204

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wetlands.n03.ctsm5.4.044: Wetlands update to ctsm5.4.044

wetlands.n04.ctsm5.4.044: Change seasonal deciduous onset

Update submodules to the latest needed for cesm3_0_alpha10a

Update submodules: ccs_config, cime, cdeps, cmeps, share
Current latest submodules that will be coming in cesm3_0_beta10

cesm3_0_beta09 had: cime6.4.1, share1.0.21, cdeps1.0.101, cmeps1.1.54

Also fix the two multi-instance tests that were failing, by making sure DGLC couples less times than ROF.

And add new ctsm_release testlist which runs every test. And make sure the list of tests that should be subsets of aux_clm or ctsm_sci are so (as well as fates, and crop_cal). And bring in a script that checks the testlist for these features and will also fix them. And bring that script into a github workflow so the testlist is checked for basic requirements.

wetlands.n04.ctsm5.4.054: Merge master 20260901 to wetlands

Add temporal smoothing of DYNBAL conservation correction fluxes

Spread the DYNBAL water and energy fluxes over many years: Rather than releasing all of
the DYNBAL fluxes in the year in which they're generated, instead put them in storage
pools that are released with a 20-year residence time (controllable via a new namelist
parameter; the default for CLM50 is set to 0.75 to maintain something closer to the old
behavior). This reduces these fluxes, especially in the oscillatory case that is somewhat
common with a dynamic ice sheet.

The new storage pools are reset when reset_dynbal_baselines is set to .true., since this
feels conceptually similar to the other resetting done by that flag, so it feels
appropriate to do this resetting at the same time.

This tag also changes the sign convention for the DYNBAL fluxes: the previous sign
convention was unintuitively the opposite of the sign convention of other fluxes to
river/atm; while I'm changing these fluxes anyway, I'm also flipping the sign convention
to be more intuitive and hopefully less error-prone.

The motivation for this change is: When subgrid areas change due to dynamic landunits /
columns, fluxes are generated to compensate for changes in gridcell-average water and
energy (QFLX_LIQ_DYNBAL, QFLX_ICE_DYNBAL, EFLX_DYNBAL). These fluxes can (and should) be
reduced via careful setting of reset_dynbal_baselines, but that still doesn't reduce these
fluxes to zero. The previous implementation seems good enough in situations where there is
a gradual change in a given grid cell's subgrid areas over many years. Unfortunately,
though, that is not always the situation when coupling to CISM, as has been seen in recent
CESM3 runs: In grid cells around the ice sheet margin, large fractions of a CTSM grid cell
can blink between mostly-vegetated/bare and mostly-glacier on a 2-year cycle, and this
oscillatory behavior can go on for many years, possibly indefinitely. This can lead to
large dynbal fluxes in each year, even when dribbled throughout the year (as was
previously done). It is problematic for the ocean to get negative dynbal fluxes, but it is
also problematic to remove these negative dynbal fluxes by spreading them globally, as is
currently done, because then regional fluxes that should average to 0 spatially and
temporally (e.g., into the Arctic ocean) end up being biased positive. This PR implements
a relatively easy partial fix, which particularly addresses the oscillatory case that
seems to be a common cause of the observed ice runoff. See
ESCOMP#4188 for more details.