The Growth of Atmospheric Droplets

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Aerosols".

Deadline for manuscript submissions: closed (31 May 2019) | Viewed by 4951

Special Issue Editor


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Guest Editor
Department of Chemical and Biomolecular Engineering, University of Maryland, College Park, MD, USA
Interests: fog; haze; visibility; cloud condensation nuclei; droplets; clouds; particle water-uptake; hygroscopicity; particle growth factors

Special Issue Information

Dear Colleagues,

Atmospheric particulate matter provides the surfaces for water-vapor to condense and form droplets. These liquid droplets can lead to the formation of fog and cloud formation. The swelling of particles is known to reduce regional visibility and thus droplet formation is key to understanding both air quality and climate. Researchers employ several methods across multiple scales to understand particle water-uptake, hygrosocopicity and droplet growth; examples include direct ambient measurements, well-constrained laboratory studies, or the construction of complex thermodynamic and kinetic models.

For this Special Issue, we aim to provide the community a valuable resource by organizing the most recent contributions to the study of aerosol droplets. Such creative works may take the form of exceptional literature review articles that outline recent developments in the field. Alternatively, authors may describe the development and application of novel measurement methods for study of atmospheric droplets. Additional contributions might include manuscripts that focus on summary ambient measurements and/or the transformation of particle properties during atmospheric processing. Lastly, laboratory and modeling studies are welcome contributions to this Special Issue. In short, all contributions that improve our understanding of atmospheric droplets are welcome.

Dr. Akua A. Asa-Awuku
Guest Editor

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Keywords

  • CCN, HTDMA, EDB, optical measurement
  • laboratory experiments
  • ambient measurements and field studies
  • thermodynamic and kinetic modelin

Published Papers (1 paper)

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Research

11 pages, 2048 KiB  
Article
A Case Study of Stratus Cloud Properties Using In Situ Aircraft Observations over Huanghua, China
by Chuanfeng Zhao, Lijun Zhao and Xiaobo Dong
Atmosphere 2019, 10(1), 19; https://doi.org/10.3390/atmos10010019 - 08 Jan 2019
Cited by 48 | Viewed by 4703
Abstract
Cloud liquid water content (LWC) and droplet effective radius (re) have an important influence on cloud physical processes and optical characteristics. The microphysical properties of a three-layer pure liquid stratus were measured by aircraft probes on 26 April 2014 over a [...] Read more.
Cloud liquid water content (LWC) and droplet effective radius (re) have an important influence on cloud physical processes and optical characteristics. The microphysical properties of a three-layer pure liquid stratus were measured by aircraft probes on 26 April 2014 over a coastal region in Huanghua, China. Vertical variations in aerosol concentration (Na), cloud condensation nuclei (CCN) at supersaturation (SS) 0.3%, cloud LWC and cloud re are examined. Large Na in the size range of 0.1–3 μm and CCN have been found within the planetary boundary layer (PBL) below ~1150 m. However, Na and CCN decrease quickly with height and reach a level similar to that over marine locations. Corresponding to the vertical distributions of aerosols and CCN, the cloud re is quite small (3.0–6 μm) at heights below 1150 m, large (7–13 μm) at high altitudes. In the PBL cloud layer, cloud re and aerosol Na show a negative relationship, while they show a clear positive relationship in the upper layer above PBL with much less aerosol Na. It also shows that the relationship between cloud re and aerosol Na changes from negative to positive when LWC increases. These results imply that the response of cloud re to aerosol Na depends on the combination effects of water-competency and collision-coalescence efficiency among droplets. The vertical structure of aerosol Na and cloud re implies potential cautions for the study of aerosol-cloud interaction using aerosol optical depth for cloud layers above the PBL altitude. Full article
(This article belongs to the Special Issue The Growth of Atmospheric Droplets)
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