Simulation of Latent Heating Rate From the Microphysical Process Associated With Mesoscale Convective System Over Korean Peninsula
Open Access
- 19 September 2022
- journal article
- research article
- Published by American Geophysical Union (AGU) in Earth and Space Science
- Vol. 9 (9)
Abstract
To investigate the structure of latent heating rate during different stages of mesoscale convective system (MCS) over the Korean Peninsula, a four nested domain Weather Research and Forecasting (WRF) model simulation with two‐way nesting method has performed. Advanced physics options from the Korean Integrated model physics are considered for simulation. Latent heating rate associated with condensation, evaporation, deposition, sublimation, freezing and melting process is computed based on different microphysical process using WRF double moment (WDM6) microphysics scheme. During the development/mature stage of the convective system, the warming associated with latent heat release by condensation is dominant below 400 hPa, and deposition above 500 hPa. The maximum contribution of warming processes from condensation, cloud nucleation, graupel accretion, and ice, snow deposition is evident. Cooling processes from rain, cloud evaporation followed by graupel, and snow melting are also noticed. Major updrafts associated with ascent of air parcel and large hydrometeor distribution is apparent along with downdrafts in the lower levels. In the dissipating stage, the cooling due to latent heat absorption by evaporation below 600 hPa and melting around 600 hPa are dominant. Contribution from cooling processes is dominant with major downdraft motion in the lower levels corresponding to the hydrometeor fall velocity. Dominant positive (negative) total latent heating provided (restrained) the energy for convection during developing and dissipating stages of system. Varied distribution of total cloud hydrometeors in different stages is apparent. Consistency between cloud hydrometeors, net heating rates, major upward (downward) motion and corresponding rainfall in developing (dissipating) stages of MCS is noticed. Model simulated latent heating (WDM6) profiles are consistent with computed moisture source and sink terms (ERA5).Keywords
This publication has 65 references indexed in Scilit:
- Latent Heating and Mixing due to Entrainment in Tropical Deep ConvectionJournal of the Atmospheric Sciences, 2014
- Microphysics of Premonsoon and Monsoon Clouds as Seen from In Situ Measurements during the Cloud Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX)Journal of the Atmospheric Sciences, 2011
- Relating Convective and Stratiform Rain to Latent HeatingJournal of Climate, 2010
- Sensitivity Study of Cloud-Resolving Convective Simulations with WRF Using Two Bulk Microphysical Parameterizations: Ice-Phase Microphysics versus Sedimentation EffectsJournal of Applied Meteorology and Climatology, 2009
- The Development and Structure of an Oceanic Squall-Line System during the South China Sea Monsoon ExperimentMonthly Weather Review, 2005
- A Study of the Response of Deep Tropical Clouds to Large-Scale Thermodynamic Forcings. Part I: Modeling Strategies and Simulations of TOGA COARE Convective SystemsJournal of the Atmospheric Sciences, 2002
- Mesoscale Convective System over the Yellow Sea - A Numerical Case StudyMeteorology and Atmospheric Physics, 1999
- An Algorithm to Estimate the Heating Budget from Vertical Hydrometeor ProfilesJournal of Applied Meteorology and Climatology, 1990
- Numerical Study of Convection Observed during the Winter Monsoon Experiment Using a Mesoscale Two-Dimensional ModelJournal of the Atmospheric Sciences, 1989
- Observational and Numerical Study of a Microburst Line-Producing StormJournal of the Atmospheric Sciences, 1989