Due to increased aerosol emissions and unfavorable weather conditions, severe haze events have occurred frequently in China in the last 10 years. In addition, the interaction between the boundary layer and the aerosol radiative effect may be another important factor in haze formation. To better understand the effect of this interaction, the aerosol radiative effect on a severe haze episode that took place in December 2013 was investigated by using two WRFChem model simulations with different aerosol configurations. The results showed that the maximal reduction of regional average surface shortwave radiation, latent heat, and sensible heat during this event were 88, 12, and 37 W m~(–2), respectively. The planetary boundary layer height, daytime temperature, and wind speed dropped by 276 m, 1°C,and 0.33 m s~(–1), respectively. The ventilation coefficient dropped by 8%–24% for in the central and northwestern Yangtze River Delta(YRD). The upper level of the atmosphere was warmed and the lower level was cooled, which stabilized the stratification. In a word, the dispersion ability of the atmosphere was weakened due to the aerosol radiative feedback. Additional results showed that the PM_(2.5) concentration in the central and northwestern YRD increased by 6–18 μg m~(–3), which is less than 15% of the average PM_(2.5) concentration during the severely polluted period in this area. The vertical profile showed that the PM_(2.5) and PM_(10) concentrations increased below 950 hPa, with a maximum increase of 7 and 8 μg m~(–3), respectively. Concentrations reduced between 950 and 800 hPa, however, with a maximum reduction of 3.5 and 4.5 μg m~(–3), respectively. Generally, the aerosol radiative effect aggravated the level of pollution, but the effect was limited, and this haze event was mainly caused by the stagnant meteorological conditions. The interaction between the boundary layer and the aerosol radiative effect may have been less important than the large-scale static weather conditions for the formation of this haze episode. Due to increased aerosol emissions and unfavorable weather conditions, severe haze events have occurred in in the last 10 years. In addition, the interaction between the boundary layer and the aerosol radiative effect may be another important factor in haze formation. the effect of this interaction, the aerosol radiative effect on a severe haze episode that took place in December 2013 was investigated by using two WRFChem model simulations with different aerosol configurations. The results showed that the maximal reduction of regional average surface shortwave radiation, latent heat , and sensible heat during this event were 88, 12, and 37 W m -2, respectively. The planetary boundary layer height, daytime temperature, and wind speed dropped by 276 m, 1 ° C, and 0.33 ms ~ ( -1), respectively. The ventilation coefficient dropped by 8% -24% for in the central and northwestern Yangtze River Delta (YRD). The upper level of the atmosphere was warmed and the lower level was cooled, which stabilized the stratification. In a word, the dispersion ability of the atmosphere was weakened due to the aerosol radiative feedback. Additional results showed that PM_ (2.5) concentration in the central and northwestern YRD increased by 6- 18 μg m ~ (-3), which is less than 15% of the average PM_ (2.5) concentration during the severely polluted period in this area. The vertical profile showed that the PM_ (2.5) and PM_ (10) 950 hPa, with a maximum increase of 7 and 8 μg m -3, respectively. Concentrations reduced between 950 and 800 hPa, however, with a maximum reduction of 3.5 and 4.5 μg m -3, respectively. Generally, , the aerosol radiative effect aggravated the level of pollution, but the effect was limited, and this haze event was mainly caused by the stagnant meteorological conditions. The interaction between the boundary layer and the aerosol radiative effect may have been less important than the large- s cale static weather conditions for the formation of this haze episode.