Coupling WRF Double-Moment 6-Class Microphysics Schemes to RRTMG Radiation Scheme in Weather Research Forecasting ModelReport as inadecuate

Coupling WRF Double-Moment 6-Class Microphysics Schemes to RRTMG Radiation Scheme in Weather Research Forecasting Model - Download this document for free, or read online. Document in PDF available to download.

Advances in Meteorology - Volume 2016 2016, Article ID 5070154, 11 pages -

Research Article

Korea Institute of Atmospheric Prediction Systems KIAPS, 35 Boramae-ro 5-gil, Dongjak-gu, Seoul 70770, Republic of Korea

Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA 99354, USA

Received 22 December 2015; Revised 5 April 2016; Accepted 13 April 2016

Academic Editor: Mario M. Miglietta

Copyright © 2016 Soo Ya Bae et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


A method to explicitly calculate the effective radius of hydrometeors in the Weather Research Forecasting WRF double-moment 6-class WDM6 microphysics scheme is designed to tackle the physical inconsistency in cloud properties between the microphysics and radiation processes. At each model time step, the calculated effective radii of hydrometeors from the WDM6 scheme are linked to the Rapid Radiative Transfer Model for GCMs RRTMG scheme to consider the cloud effects in radiative flux calculation. This coupling effect of cloud properties between the WDM6 and RRTMG algorithms is examined for a heavy rainfall event in Korea during 25–27 July 2011, and it is compared to the results from the control simulation in which the effective radius is prescribed as a constant value. It is found that the derived radii of hydrometeors in the WDM6 scheme are generally larger than the prescribed values in the RRTMG scheme. Consequently, shortwave fluxes reaching the ground SWDOWN are increased over less cloudy regions, showing a better agreement with a satellite image. The overall distribution of the 24-hour accumulated rainfall is not affected but its amount is changed. A spurious rainfall peak over the Yellow Sea is alleviated, whereas the local maximum in the central part of the peninsula is increased.

Author: Soo Ya Bae, Song-You Hong, and Kyo-Sun Sunny Lim



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