An unprecedented heavy rainfall event in China (“21.7” extreme rainfall event) was simulated using the global variable-resolution model (MPAS-Atmosphere) across the scales (4km, 8km, 16km and 50km). Although almost all experiments at different resolutions reproduce the spatiotemporal characteristics of precipitation, the precipitation intensity simulated by the experiment at 16 km is closest to the observations, and gradually decrease form 8 km, 50 km to 4 km. Precipitation magnitude is prominently influenced by the difference in simulated large-scale circulation across a range of grid spacings. Further analysis revealed that the differences in latent heating across scales affect the geopotential height and wind field by altering temperature. The latent heating in 4km simulation is the minimum while the 16km simulation is maximum. More latent heating release leads to the low-level pressure depression, amplifies the water vapor flux convergence, produces stronger upward motion and more clouds, and ultimately results in stronger precipitation. The sensitivity experiments for turning off latent heating tendencies during the event showed that the latent heat release has positive feedback on the "21.7" heavy rainfall event. This study suggests that the difference in simulated latent heat release during the event is the main reason for simulated different atmospheric circulation and precipitation across scales.

global variable-resolution model,heavy precipitation,resolution