A numerical study of aerosol influence on mixed-phase stratiform clouds through modulation of the liquid phase

被引:13
作者
de Boer, G. [1 ,2 ,3 ]
Hashino, T. [4 ]
Tripoli, G. J. [5 ]
Eloranta, E. W. [5 ]
机构
[1] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[2] NOAA, Earth Syst Res Lab, Div Phys Sci, Boulder, CO USA
[3] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Div Earth Sci, Berkeley, CA 94720 USA
[4] Univ Tokyo, Atmosphere & Ocean Res Inst, Chiba, Japan
[5] Univ Wisconsin, Dept Atmospher & Ocean Sci, Madison, WI USA
基金
美国国家科学基金会; 美国能源部; 美国国家航空航天局; 美国海洋和大气管理局;
关键词
ICE NUCLEATION; CONDENSATION NUCLEI; IMMERSION MODE; PARTICLES; MICROPHYSICS; SENSITIVITY; HEAT; SIMULATION; VAPOR; CCN;
D O I
10.5194/acp-13-1733-2013
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Numerical simulations were carried out in a high-resolution two-dimensional framework to increase our understanding of aerosol indirect effects in mixed-phase stratiform clouds. Aerosol characteristics explored include insoluble particle type, soluble mass fraction, influence of aerosol-induced freezing point depression and influence of aerosol number concentration. Simulations were analyzed with a focus on the processes related to liquid phase microphysics, and ice formation was limited to droplet freezing. Of the aerosol properties investigated, aerosol insoluble mass type and its associated freezing efficiency was found to be most relevant to cloud lifetime. Secondary effects from aerosol soluble mass fraction and number concentration also alter cloud characteristics and lifetime. These alterations occur via various mechanisms, including changes to the amount of nucleated ice, influence on liquid phase precipitation and ice riming rates, and changes to liquid droplet nucleation and growth rates. Alteration of the aerosol properties in simulations with identical initial and boundary conditions results in large variability in simulated cloud thickness and lifetime, ranging from rapid and complete glaciation of liquid to the production of long-lived, thick stratiform mixed-phase cloud.
引用
收藏
页码:1733 / 1749
页数:17
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