Abstract
Simulations of mesoscale convective systems (MCSs) are conducted using the Weather Research and Forecasting (WRF) model. The considered MCSs occurred on 13 and 14 April 2016 over the west and southwest of Iran and resulted in a heavy flood. To determine the appropriate cumulus parameterization scheme to run the model, simulations of the two MCSs were performed using four nesting domains with 36-, 12-, 4-, and 1.33-km horizontal resolution by examining five cumulus parameterization schemes (CPSs) available in the WRF model for the three outer domains. The five implemented CPSs tested include Kain–Fritsch (KF), Betts–Miller–Janjic (BMJ), Grell–Devenyi (GD), improved Grell–Devenyi (G3D), and Grell–Freitas (GF) schemes. Initial fields for the simulations are taken from the Final Global Analysis (FNL) data with 1-degree horizontal resolution at 6-h time intervals. The simulations were evaluated using two available observational data sets: the Global Precipitation Measurement (GPM) satellite and synoptic station data. Comparison of the simulated 24-hourly precipitation from the second domain of the simulations (12 km) against the GPM data showed that the BMJ and GF schemes have the best performance in the simulation of 24-hourly precipitation based on the minimum values of root-mean-square error (RMSE). The comparison between in situ and the simulated precipitation from the third domain with 4-km resolution shows the great success of the GF scheme in predicting precipitation for 2 consecutive days. Regarding the dynamical analysis of the MCS of 13 April 2016, results of the simulation with 1.33-km resolution (using the GF scheme for the three outer domains) suggest that the model can explain several characteristics such as (1) the horizontal pattern of the MCS, including the convective line and stratiform precipitation region, (2) the formation of an elevated unstable moist layer and its slantwise ascent to the rear of the system, (3) the vertical structure of the MCS, and (4) the formation of a rear inflow jet and its descent to the surface under the influence of cooling processes below the stratiform cloud base.
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The authors would like to thank Dr. Alireza Mahmoudian for his help in editing the manuscript.
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Ahmadloo, M., Gharaylou, M., Farahani, M.M. et al. Simulation and Analysis of Mesoscale Convective Systems (MCSs) Leading to a Severe Flood Over Iran. Pure Appl. Geophys. 179, 1485–1507 (2022). https://doi.org/10.1007/s00024-022-02983-4
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DOI: https://doi.org/10.1007/s00024-022-02983-4