2020
DOI: 10.1029/2019jd030756
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Systematic Bias in the Prediction of Warm‐Rain Hydrometeors in the WDM6 Microphysics Scheme and Modifications

Abstract: Modifications are made to the calculation of warm‐rain hydrometeor number concentrations of the Weather Research and Forecasting double‐moment six‐class (WDM6) microphysics scheme. These modifications are related with cloud condensation nuclei activation, cloud droplet evaporation, and snow and graupel melting. The effects of the modifications are tested in a North China heavy rain event (Case01) as well as a short‐duration rain event in Hebei Province of China (Case02). The results show that the WDM6 scheme u… Show more

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Cited by 22 publications
(14 citation statements)
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“…In addition, it is also notable in the vertical reflectivity profiles (Figure 8) that BULK scheme shows abnormally lower simulated values than the observed near the melting level, which can partially explain its poorer performances than BIN scheme in simulating warm rain processes. As reported in Lei et al [53], BULK scheme (WDM6 scheme) has systematic bias in the prediction of warm rain hydrometeors, and high concentration of small raindrops tends to appear near the 0 • C layer as validated against airborne observations. To confirm that, we give the number concentration of warm rain hydrometeors in typhoon simulations as shown in Figure 12.…”
Section: Discussionsupporting
confidence: 56%
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“…In addition, it is also notable in the vertical reflectivity profiles (Figure 8) that BULK scheme shows abnormally lower simulated values than the observed near the melting level, which can partially explain its poorer performances than BIN scheme in simulating warm rain processes. As reported in Lei et al [53], BULK scheme (WDM6 scheme) has systematic bias in the prediction of warm rain hydrometeors, and high concentration of small raindrops tends to appear near the 0 • C layer as validated against airborne observations. To confirm that, we give the number concentration of warm rain hydrometeors in typhoon simulations as shown in Figure 12.…”
Section: Discussionsupporting
confidence: 56%
“…To confirm that, we give the number concentration of warm rain hydrometeors in typhoon simulations as shown in Figure 12. One can notice that BULK scheme (WDM7 scheme) produces abnormally high raindrop number concentrations at an altitude around the melting level (Figure 12a), possibly due to the fast melting processes of snow, graupel, and hail [53]. Meanwhile, the cloud drop number concentrations of BULK scheme are significantly higher than that of BIN scheme (Figure 12b), probably because of the saturation adjustment strategy in BULK scheme.…”
Section: Discussionmentioning
confidence: 99%
“…In this study, we considered operational configurations of KLAPS, such as the RRTMG-K radiation (Baek, 2017) and WRF double moment 7-Class (WDM7) microphysics (Bae et al, 2019), Shin and Hong planetary boundary layer (Shin & Hong, 2015), KIAPS Simplified Arakawa-Schubert (SAS) cumulus (Kwon & Hong, 2017), Unified Noah land surface model (Tewari et al, 2004), and revised MM5 Monin-Obukhov surface layer (Jiménez et al, 2012). The systemic biases for the WDM7 microphysics scheme, which were reported by Lei et al (2020), were corrected in this study. Although the KLAPS also includes a local data assimilation system, it was replaced with the use of European Centre for Medium-Range Weather Forecasts Reanalysis v5 (ERA5) data (Hersbach et al, 2020) in the WRF Preprocessing System.…”
Section: Methodsmentioning
confidence: 99%
“…The KF scheme is used only in the outer domain (9 km). The WDM7 cloud microphysics scheme [10] with the bug fix from Lei et al [32] is applied. The cloud microphysics processes in WDM7 are recoded to allow WDM7 to adopt the observed microphysical parameters during the ICE-POP 2018 field campaign.…”
Section: Model Configurationmentioning
confidence: 99%