An Evaluation of WRF Microphysics Schemes for Simulating the Warm-Type Heavy Rain over the Korean Peninsula

• Published in: Asia-Pacific journal of atmospheric sciences Vol. 54; no. 2; pp. 225 - 236
• Main Authors: Song, Hwan-Jin, Sohn, Byung-Ju
• Format: Journal Article
• Language: English
• Published: Seoul Korean Meteorological Society 01.05.2018; Springer Nature B.V; 한국기상학회
• Subjects: Atmospheric precipitations; Atmospheric Sciences; Climatology; Cloud microphysics; Cloud systems; Coalescence; Convection; Earth and Environmental Science; Earth Sciences; Evaluation; Geophysics/Geodesy; Heavy rainfall; Melting; Meteorological satellites; Microphysics; Moisture content; Parameterization; Precipitation; Profiles; Radar; Rain; Rainfall; Rainfall simulators; Reflectance; Satellite observation; Satellites; Storms; Tropical climate; Tropical rainfall; Tropical Rainfall Measuring Mission (TRMM); Vertical profiles; Water content; Weather forecasting; 대기과학; precipitation; TRMM; WRF; warm-type; WDM6; heavy rainfall
• ISSN: 1976-7633; 1976-7951
• DOI: 10.1007/s13143-018-0006-2

The Korean peninsula is the region of distinctly showing the heavy rain associated with relatively low storm height and small ice water content in the upper part of cloud system (i.e., so-called warm-type heavy rainfall). The satellite observations for the warm-type rain over Korea led to a conjecture that the cloud microphysics parameterization suitable for the continental deep convection may not work well for the warm-type heavy rainfall over the Korean peninsula. Therefore, there is a growing need to examine the performance of cloud microphysics schemes for simulating the warm-type heavy rain structures over the Korean peninsula. This study aims to evaluate the capabilities of eight microphysics schemes in the Weather Research and Forecasting (WRF) model how warm-type heavy rain structures can be simulated, in reference to the Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (PR) reflectivity measurements. The results indicate that the WRF Double Moment 6-class (WDM6) scheme simulated best the vertical structure of warm-type heavy rain by virtue of a reasonable collision-coalescence process between liquid droplets and the smallest amount of snow. Nonetheless the WDM6 scheme appears to have limitations that need to be improved upon for a realistic reflectivity structure, in terms of the reflectivity slope below the melting layer, discontinuity in reflectivity profiles around the melting layer, and overestimation of upper-level reflectivity due to high graupel content.