Abstract

A heavy rainstorm occurred in Beijing on 19–20 July 2016. The Weather Research and Forecasting Model coupled with Chemistry (WRF-Chem) was used to investigate the effects of anthropogenic aerosols on precipitation and microphysical processes. Three conditions were simulated by altering the anthropogenic emissions. When the anthropogenic emissions were increased by 10 times, the area-average accumulated rainfall amount and maximum accumulated rainfall amount both decreased. The cloud water mixing ratio increased and the rain mixing ratio decreased. The radii of cloud droplets decreased, and the collision efficiency of cloud water by rain and the autoconversion rate of cloud water into rain were both low. When the anthropogenic emission was 10% of the original emission, the area of accumulated rainfall amounts greater than 25 mm in the Beijing area was 10% larger than those of the other two tests. The collision efficiency and autoconversion rate of cloud water into rain were high for large contact areas and large cloud droplets. The graupel mixing ratio was the largest. Thus, the process of melting of graupel into rain was the largest. In the WRF-Chem model, the aerosols did not participate as ice nuclei (IN) in the ice-phase microphysical processes, and therefore the aerosols could influence only the warm rain processes and mix-phased processes near the freezing level line. For no influence on ice-phase microphysical processes, the snow and ice mixing ratios did not show many differences among the different tests.

Highlights

  • With rapid economic development, the population increases dramatically, and urbanization issues become increasingly prominent

  • A heavy rainstorm occurred in Beijing on 19–20 July, 2016

  • The WRF-Chem model was used to investigate the effects of aerosols on precipitation and microphysical processes by altering the anthropogenic emission

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Summary

Introduction

The population increases dramatically, and urbanization issues become increasingly prominent. Atmosphere 2019, 10, 162 research on aerosols, the way aerosols affect clouds and precipitation directly and indirectly keeps a lot of uncertainties [20,21,22]. It varies under different weather conditions and areas, and it has a very complicated mechanism, resulting from the interactions among thermal, dynamic, and microphysical processes [23,24]. The researchers found that the variation in aerosol concentrations had significant effects on the cloud microphysical processes, as well as on hail precipitation during hailstorms at the surface. Gibbons et al [37] studied the effects of dust aerosols on precipitation using bin microphysical schemes coupled with the WRF model.

The Precipitation Event
19 July Standard
Model Setup
Experimental Design
Results
The variations
19 July to 0800
Effects of Aerosols on Microphysical Processes
Effects
Conclusions
Full Text
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