Two small fixes in Thompson MP based on CCPP code with UFS testing#1894
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TYPE: bug fix KEYWORDS: microphysics, Thompson, CCPP SOURCE: gthompsn DESCRIPTION OF CHANGES: As described in UFS PR69 there are two changes for Thompson-MP: 1. The minimum size of snow was increased (some months ago) but it was noted that the min size of snow is used to determine the upper-most size bin of cloud ice. It was set to 5 times the min size of snow, which is exceedingly large for the cloud ice category. Therefore, the constant was reduced to 2 - making cloud ice largest size bin of 600 microns which is plenty big enough, giving more resolution to all the ice size bins. 2. In testing RRFS with @ericaligo-NOAA and @RuiyuSun for a specific case study, it was noted that rain was evaporating with a large rate producing a temperature tendency of 27C/hour. We traced the issue to an extremely large number of rain drops that appears to be produced by colliding rain and graupel - which has an explicit drop breakup (splash if you will) from the collisions making 5 drops per collision. This was forcing the rain (formed by melting graupel) to tends towards 500 microns (0.5 mm) which is too small. So the constant used for collisions was reduced to 1.5 in an effort to keep rain larger (thus reducing evaporation). The third bullet of the referenced UFS PR is irrelevant because the values of prr_sml and prr_gml are held to zero instead of negative with the MAX statement. LIST OF MODIFIED FILES: module_mp_thompson.F only TESTS CONDUCTED: 1. Tested in RRFS and GFS but not in WRF. The result of bullet 2 above will cause large rain drops so changes to simulations are expected. 2. The Jenkins tests are all passing. RELEASE NOTE: Based on testing within CCPP version of the scheme for UFS (both RRFS and GFS), two minor changes to the Thompson microphysics scheme were added here.
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Based on testing within CCPP for UFS (both RRFS and GFS), two minor updates to the Thompson microphysics scheme.
TYPE: bug fix
KEYWORDS: microphysics, Thompson, CCPP
SOURCE: gthompsn
DESCRIPTION OF CHANGES:
As described in UFS PR69 there are two changes for Thompson-MP:
The minimum size of snow was increased (some months ago) but it was noted that the min size of snow is used to determine the upper-most size bin of cloud ice. It was set to 5 times the min size of snow, which is exceedingly large for the cloud ice category. Therefore, the constant was reduced to 2 - making cloud ice largest size bin of 600 microns which is plenty big enough, giving more resolution to all the ice size bins.
In testing RRFS with @ericaligo-NOAA and @RuiyuSun for a specific case study, it was noted that rain was evaporating with a large rate producing a temperature tendency of 27C/hour. We traced the issue to an extremely large number of rain drops that appears to be produced by colliding rain and graupel - which has an explicit drop breakup (splash if you will) from the collisions making 5 drops per collision. This was forcing the rain (formed by melting graupel) to tends towards 500 microns (0.5 mm) which is too small. So the constant used for collisions was reduced to 1.5 in an effort to keep rain larger (thus reducing evaporation).
The third bullet of the referenced UFS PR is irrelevant because the values of
prr_smlandprr_gmlare held to zero instead of negative with theMAXstatement.LIST OF MODIFIED FILES:
module_mp_thompson.FonlyTESTS CONDUCTED:
Tested in RRFS and GFS but not in WRF. The result of bullet 2 above will cause large rain drops so changes to simulations are expected.
RELEASE NOTE: Minor changes to Thompson-MP aligning with changes made in CCPP for use in UFS.