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DOI10.5194/acp-21-16843-2021
Midlatitude mixed-phase stratocumulus clouds and their interactions with aerosols: how ice processes affect microphysical, dynamic, and thermodynamic development in those clouds and interactions?
Lee S.S.; Ha K.-J.; Manoj M.G.; Kamruzzaman M.; Kim H.; Utsumi N.; Zheng Y.; Kim B.-G.; Jung C.H.; Um J.; Guo J.; Choi K.O.; Kim G.-U.
发表日期2021
ISSN1680-7316
起始页码16843
结束页码16868
卷号21期号:22
英文摘要Midlatitude mixed-phase stratocumulus clouds and their interactions with aerosols remain poorly understood. This study examines the roles of ice processes in those clouds and their interactions with aerosols using a large-eddy simulation (LES) framework. Cloud mass becomes much lower in the presence of ice processes and the Wegener-Bergeron-Findeisen (WBF) mechanism in the mixed-phase clouds compared to that in warm clouds. This is because while the WBF mechanism enhances the evaporation of droplets, the low concentration of aerosols acting as ice-nucleating particles (INPs) and cloud ice number concentration (CINC) prevent the efficient deposition of water vapor. Note that the INP concentration in this study is based on the observed spatiotemporal variability of aerosols. This results in the lower CINC compared to that with empirical dependence of the INP concentrations on temperature in a previous study. In the mixed-phase clouds, the increasing concentration of aerosols that act as cloud condensation nuclei (CCN) decreases cloud mass by increasing the evaporation of droplets through the WBF mechanism and decreasing the intensity of updrafts. In contrast to this, in the warm clouds, the absence of the WBF mechanism makes the increase in the evaporation of droplets inefficient, eventually enabling cloud mass to increase with the increasing concentration of aerosols acting as CCN. Here, the results show that when there is an increasing concentration of aerosols that act as INPs, the deposition of water vapor is more efficient than when there is the increasing concentration of aerosols acting as CCN, which in turn enables cloud mass to increase in the mixed-phase clouds. © 2021 Seoung Soo Lee et al.
语种英语
来源期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/246430
作者单位Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, United States; Research Center for Climate Sciences, Pusan National University, Busan, South Korea; Center for Climate Physics, Institute for Basic Science, Busan, South Korea; BK21 School of Earth and Environmental Systems, Pusan National University, Busan, South Korea; Advanced Centre for Atmospheric Radar Research, Cochin University of Science and Technology, Kerala, India; School of Mathematical Sciences, University of Adelaide, Adelaide, Australia; Natural and Built Environments Research Centre, Division of Information Technology Engineering and the Environment (ITEE), University of South Australia, Adelaide, Australia; Institute of Industrial Science, University of Tokyo, Tokyo, Japan; Moon Soul Graduate School of Future Strategy, Korea Advanced Institute of Science and Technology, Daejeon, South Korea; Department of Civil and Environmental Engineering, Korea Advanced Institute of Science and Technology, Daejeon...
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Lee S.S.,Ha K.-J.,Manoj M.G.,et al. Midlatitude mixed-phase stratocumulus clouds and their interactions with aerosols: how ice processes affect microphysical, dynamic, and thermodynamic development in those clouds and interactions?[J],2021,21(22).
APA Lee S.S..,Ha K.-J..,Manoj M.G..,Kamruzzaman M..,Kim H..,...&Kim G.-U..(2021).Midlatitude mixed-phase stratocumulus clouds and their interactions with aerosols: how ice processes affect microphysical, dynamic, and thermodynamic development in those clouds and interactions?.ATMOSPHERIC CHEMISTRY AND PHYSICS,21(22).
MLA Lee S.S.,et al."Midlatitude mixed-phase stratocumulus clouds and their interactions with aerosols: how ice processes affect microphysical, dynamic, and thermodynamic development in those clouds and interactions?".ATMOSPHERIC CHEMISTRY AND PHYSICS 21.22(2021).
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