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DOI | 10.5194/acp-20-5093-2020 |
The effects of cloud-aerosol interaction complexity on simulations of presummer rainfall over southern China | |
Furtado K.; Field P.; Luo Y.; Zhou T.; Hill A. | |
发表日期 | 2020 |
ISSN | 16807316 |
起始页码 | 5093 |
结束页码 | 5110 |
卷号 | 20期号:8 |
英文摘要 | Convection-permitting simulations are used to understand the effects of cloud-aerosol interactions in a case of heavy rainfall over southern China. The simulations are evaluated using radar observations from the Southern China Monsoon Rainfall Experiment (SCMREX) and remotely sensed estimates of precipitation, clouds and radiation. We focus on the effects of complexity in cloud-aerosol interactions, especially the depletion and transport of aerosol material by clouds. In particular, simulations with aerosol concentrations held constant are compared with a fully cloud-aerosol-interacting system to investigate the effects of two-way coupling between aerosols and clouds on a line of organised deep convection. It is shown that the cloud processing of aerosols can change the vertical structure of the storm by using up aerosols within the core of line, thereby maintaining a relatively clean environment which propagates with the heaviest rainfall. This induces changes in the statistics of surface rainfall, with a cleaner environment being associated with less-intense but more-frequent rainfall. These effects are shown to be related to a shortening of the timescale for converting cloud droplets to rain as the aerosol number concentration is decreased. The simulations are compared to satellite-derived estimates of surface rainfall, a condensed-water path and the outgoing flux of short-wave radiation. Simulations for fewer aerosol particles outperform the more polluted simulations for surface rainfall but give poorer representations of top-of-atmosphere (TOA) radiation. © 2020 BMJ Publishing Group. All rights reserved. |
关键词 | aerosolatmospheric transportclimate effectclimate forcingcloud microphysicscomplexitycomputer simulationconcentration (composition)convective systemnumerical modelrainfalltop of atmosphereChina |
语种 | 英语 |
来源机构 | Atmospheric Chemistry and Physics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/132068 |
推荐引用方式 GB/T 7714 | Furtado K.,Field P.,Luo Y.,et al. The effects of cloud-aerosol interaction complexity on simulations of presummer rainfall over southern China[J]. Atmospheric Chemistry and Physics,2020,20(8). |
APA | Furtado K.,Field P.,Luo Y.,Zhou T.,&Hill A..(2020).The effects of cloud-aerosol interaction complexity on simulations of presummer rainfall over southern China.,20(8). |
MLA | Furtado K.,et al."The effects of cloud-aerosol interaction complexity on simulations of presummer rainfall over southern China".20.8(2020). |
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