CPT tuning effort #212
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Colin provided some preliminary plots of output here: "x021 runs = cam_dev In x222 runs ("new") runs, that increase in precip near the equator appears to be due to lower ZM% and therefore more precip from PUMAS (see FREQZM and PRECZM_FRACTION). x222 runs also has lower CAPE, but more CLDLOW and total cloud water path. So for "taus + upwp" (untuned!) in the tropics, cloudier, (slightly) more stable, clouds are more bottom-heavy, PUMAS rains more vs. ZM. AMWG diags here. |
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Vince and I looked at some tuner plots this morning. C_uu_shr has a small value in the default run---we could try a run with a larger value of C_uu_shr (maybe 0.5) and see what that does. We could also try a few additional runs extending the range of C_uu_shr for the tuner. c_uu_shr = 0.225 so we could try that. This seemed to help a lot with Hawaii, DYCOMS, and VOCALS. These numbers came from tuning C_uu_shr, gamma_coef, altitude_threshold, and c_invrs_tau_shear, with DYCOMS and VOCALS weighted 4 and Hawaii weighted 8 (globals weighted 12). Since this was a first effort, probably worth looking at the ranges of all the parameters and consider whether they should be extended, etc. |
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Met w/ Vince 1/25/23. Vince says do a run with and without taus and then do the AMWG diagnostics model v model and Zhun's plots too. Model v model plots may contain omega comparison. Need to figure out why it's going deep in eastern Pacific; check CLUBB's wp2 variable in this connection. What's going on over DYCOMS region in the profile plots? Also compare the red and blue arrows in Zhun's tuner plots (requires processing the new runs with the diagnostics code). |
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I used Zhun's tuner with a set of parameters that was supposed to improve DYCOMS and the eastern Pacific (EP), with Hawaii weighted at a medium value, and here are the results from that run (zt14) compared to obs and compared to my default (zt0) run (link for that one above). The eastern Pacific did improve but DYCOMS and Hawaii got worse, and went in the opposite direction from what the tuner predicted (why?). In other words, things dimmed in the EP as desired, but this also dimmed Sc which is the opposite of what we want. zt14 minus obs: zt14 minus zt0: |
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I talked with @swrneale the other day about how to possibly get ZM to be less active in the eastern Pacific (EP)---a look at some profile plots does suggest that omega is too strong in this region and things are too cloudy, but CLUBB is mostly active near the surface so presumably this is mainly related to ZM---and his first suggestion was to set the flag zmconv_parcel_pbl = .false., which is normally true by default for runs using cam_development. Here is the output of that run (this link includes both comparison to obs and comparison to my default zt0 run). https://webext.cgd.ucar.edu/F2000climo/zt11/atm/ This flag does not seem to have had much impact in the deep tropical EP, but did brighten things up by a few W/m2 in the global mean. @swrneale do you have other suggestions for things to modify within ZM that might help to dim the EP? |
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@bstephens82 this is a challenge as the entrainment rate and stability are cranked up to probably their highest level. Do you have the climo files for the existing cam-dev 'control' and your taus code tuning effort, just so I can see how ZM contributions have changed? |
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Ben, it might be worth setting |
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I thought I would share one of my latest runs, which I call
This has strongly brightened the Sc decks (too much in the case of the South American deck), but interestingly has not greatly brightened the eastern Pacific ITCZ relative to my control (it may even look very slightly better than the control). It also has mean SWCF -46.43, which is closer to what I believe is the new CERES-EBAF number, something like -45.8 or so. Diagnostics here: |
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A couple of test I did on Friday look fairly decent I would say compared to my control case. These are still a bit too bright in the tropical EP and west of the South American coast in that region, but I would say things are looking at lot better off the coast of California. In both of these cases, I've adjusted micro_mg_dcs and micro_mg_autocon_fact on the microphys side and gamma_coef on the CLUBB side. Here are diagnostics along with comparisons to zt0 (control run). zt21: I noticed that zt20 also looks a little better with respect to surface stress: |
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@JulioTBacmeister and I looked at this recent test I did, which has some nice features, and we were wondering about ways to break up the Sc near the ITCZ, since the Sc are coming too close to the ITCZ. How can we shift these poleward? It could be that subsidence is not strong enough on the edges of the ITCZ, I'll check into that. We are also wondering if there is a correlation between surface heat flux and inversion strength at cloud top. @vlarson do you have any thoughts or suggestions about this? |
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I used the DiagnosticsAndTools plotting code to plot out three cases from the 092 tag:
The new profile plots are here. I put a grid of I think 40 points over the region that shows the persistent bright spot off of western South America, so we could get a good look at diagnostics in this area. These points are labeled "WSA" on the page that opens when you click the link for the plots. I'm still looking over these plots, but one thing that sticks out to me right away are the differences in the skewness functions. |
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@vlarson @JulioTBacmeister @adamrher @zarzycki we can put tuning-related developments here.
This link will take you to my "starting point" default run that I used with Zhun's tuner scripts: https://webext.cgd.ucar.edu/F2000climo/zt0/atm/zt0-obs.0001_1/. This run includes
These should account for most of what @Katetc is bringing in with the new external, although there may be some other minor changes to CLUBB coming in with the new external.
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