Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1002/2017JD027884 |
Parameterization of In-Cloud Aerosol Scavenging Due To Atmospheric Ionization: 2. Effects of Varying Particle Density | |
Zhang, Liang1,2; Tinsley, Brian A.2 | |
2018-03-27 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
![]() |
ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2018 |
卷号 | 123期号:6页码:3099-3115 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China; USA |
英文摘要 | Simulations and parameterization of collision rate coefficients for aerosol particles with 3m radius droplets have been extended to a range of particle densities up to 2,000kgm(-3) for midtropospheric (similar to 5km) conditions (540hPa, -17 degrees C). The increasing weight has no effect on collisions for particle radii less than 0.2m, but for greater radii the weight effect becomes significant and usually decreases the collision rate coefficient. When increasing size and density of particles make the fall speed of the particle relative to undisturbed air approach to that of the droplet, the effect of the particle falling away in the stagnation region ahead of the droplet becomes important, and the probability of frontside collisions can decrease to zero. Collisions on the rear side of the droplet can be enhanced as particle weight increases, and for this the weight effect tends to increase the rate coefficients. For charges on the droplet and for large particles with density <1,000kgm(-3) the predominant effect increases in rate coefficient due to the short-range attractive image electric force. With density above about 1,000kgm(-3), the stagnation region prevents particles moving close to the droplet and reduces the effect of these short-range forces. Together with previous work, it is now possible to obtain collision rate coefficients for realistic combinations of droplet charge, particle charge, droplet radius, particle radius, particle density, and relative humidity in clouds. The parameterization allows rapid access to these values for use in cloud models. Plain Language Summary Atmospheric electric charges affect the rate of collision with droplets of aerosol particles acting as condensation nuclei and ice-forming nuclei. This changes their concentrations and can generate primary ice, affecting the development of clouds, and explains observations of cloud and surface pressure responses to changes in atmospheric electricity. We have modeled these collision rates as functions of electric charges, particle radii and density, and relative humidity, extending previous results for a range of droplet radii. We give the results in a form easily incorporated into cloud models. |
英文关键词 | cloud microphysics electric charge particle density particle scavenging |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000430108900010 |
WOS关键词 | ELECTRIC-FIELD ; SOLAR-ACTIVITY ; PRECIPITATION ; ELECTRIFICATION ; DROPLETS ; COVER ; LINKS ; RAIN |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/32975 |
专题 | 气候变化 |
作者单位 | 1.East China Normal Univ, Inst Ecochongming, Shanghai, Peoples R China; 2.Univ Texas Dallas, Dept Phys, Richardson, TX 75083 USA |
推荐引用方式 GB/T 7714 | Zhang, Liang,Tinsley, Brian A.. Parameterization of In-Cloud Aerosol Scavenging Due To Atmospheric Ionization: 2. Effects of Varying Particle Density[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2018,123(6):3099-3115. |
APA | Zhang, Liang,&Tinsley, Brian A..(2018).Parameterization of In-Cloud Aerosol Scavenging Due To Atmospheric Ionization: 2. Effects of Varying Particle Density.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,123(6),3099-3115. |
MLA | Zhang, Liang,et al."Parameterization of In-Cloud Aerosol Scavenging Due To Atmospheric Ionization: 2. Effects of Varying Particle Density".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 123.6(2018):3099-3115. |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论