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Major updated CSAW deep convective scheme and made the CSAWMG schemes pass RTs for intel and GNU #1063
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… into feature_reorg_physics
1. adding a heat source from fires. It is icontrolled by a flag and not turned on yet. Needs more testing. 2. Adding output of surface paramteres: leaf area index (LAI), wilting point and soil field capacity.
1. Removed commented lines in fire feedback to RUC LSM. 2. The coordinates of a test point are passed to the RUC LSM subroutines to make debug printing more manageable. 3. Reverted change in the TRANSF subroutine to original version. The non-linear root distribution needs scientific evaluation in the retro runs.
@AnningCheng-NOAA it says 397 files are changed in this PR? Should it go into something more recent in the ufs-community/ccpp repo and not into NCAR main? |
Lisa, Those 397 files are likely changed after I checked out the trunk a few weeks ago. I have only modified the cs_conv.F90. There should be numerous conflicts when I merged my branches with the trunk again. |
@AnningCheng-NOAA Can you please close this PR and open it in https://github.com/ufs-community/ccpp-physics? |
closed PR was put to the wrong repo. |
Done. @dustin Swales - NOAA Federal ***@***.***> .
…On Tue, Feb 13, 2024 at 10:34 AM Dustin Swales ***@***.***> wrote:
@AnningCheng-NOAA <https://github.com/AnningCheng-NOAA> Can you please
close this PR and open it in https://github.com/ufs-community/ccpp-physics
?
(It seems from the commit log that is where you branched your work from)
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• Major updated CSAW deep convective scheme: considering sigma vertical veriantion and reduction on fluxes instead of tendency etc.
• Regression tests are performed on the new version of CSAW for GNU and intel compilers
Here is a EMail from Don describe the changes:
On Thu, Oct 24, 2019 at 3:01 PM Donald Dazlich - NOAA Affiliate <donald.dazlich@noaa.gov> wrote:
Hi Moorthi, Anning,
Dave and I have been using the GFS version of CS to redo our implementation of AW more completely and consistently. Now, you will find that the fix_form implemetation of the tendencies match up very closely with the traditional form. Also you will notice that it is the fluxes for each cloud type (and the downdraft) that are saved and the reduction is done on the fluxes, not the tendency computed from the flux divergence. Since sigma is a function of height the latter approach is incorrect. I’ve also dimensioned several cloud type variables nctp+1 - the nctp+1 slot has downdraft output. Another addition is the sorting of the lamdas after they are computed for all cloud types, then computing the sigma. This approach is detailed in a manuscript Dave is working on. Also, sigma is not applied to the inputs to the downdraft routine, but to the outputs, which are now mass fluxes not tendencies. The water and thermodynamic budgets remain satisfied now.
I’ve attached my version below. It should be pretty close to your version with regards to the interface so you shouldn’t have to do much work with it.
Regards,
Don