Negative Aerosol-Cloud re Relationship From Aircraft Observations Over Hebei, China

被引:108
作者
Zhao, Chuanfeng [1 ,2 ]
Qiu, Yanmei [1 ,2 ]
Dong, Xiaobo [3 ]
Wang, Zhien [4 ]
Peng, Yiran [5 ]
Li, Baodong [3 ]
Wu, Zhihui [3 ]
Wang, Yang [1 ,2 ]
机构
[1] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing, Peoples R China
[2] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing, Peoples R China
[3] Weather Modificat Off Hebei Prov, Shijiazhuang, Hebei, Peoples R China
[4] Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA
[5] Tsinghua Univ, Ctr Earth Syst Sci, Beijing, Peoples R China
来源
EARTH AND SPACE SCIENCE | 2018年 / 5卷 / 01期
基金
中国国家自然科学基金;
关键词
aerosol-cloud r(e) relationship; aircraft observation; aerosol first indirect effect; cloud droplet effective radius; Hebei; DROPLET EFFECTIVE RADIUS; IN-SITU OBSERVATIONS; RADIATION BUDGET; SEASONAL-VARIATION; STRATUS; MICROPHYSICS; POLLUTION; LIQUID; CLIMATE; CUMULUS;
D O I
10.1002/2017EA000346
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Using six flights observations in September 2015 over Hebei, China, this study shows a robust negative aerosol-cloud droplet effective radius (r(e)) relationship for liquid clouds, which is different from previous studies that found positive aerosol-cloud r(e) relationship over East China using satellite observations. A total of 27 cloud samples was analyzed with the classification of clean and polluted conditions using lower and upper 1/3 aerosol concentration at 200 m below the cloud bases. By normalizing the profiles of cloud droplet r(e), we found significant smaller values under polluted than under clean condition at most heights. Moreover, the averaged profiles of cloud liquid water content (LWC) show larger values under polluted than clean conditions, indicating even stronger negative aerosol-cloud r(e) relationship if LWC is kept constant. The droplet size distributions further demonstrate that more droplets concentrate within smaller size ranges under polluted conditions. Quantitatively, the aerosol-cloud interaction is found around 0.10-0.19 for the study region.
引用
收藏
页码:19 / 29
页数:11
相关论文
共 74 条
[1]  
BAUMGARDNER D, 1983, J CLIM APPL METEOROL, V22, P891, DOI 10.1175/1520-0450(1983)022<0891:AAACOF>2.0.CO
[2]  
2
[3]   Observations of the first aerosol indirect effect in shallow cumuli [J].
Berg, Larry K. ;
Berkowitz, Carl M. ;
Barnard, James C. ;
Senum, Gunnar ;
Springston, Stephen R. .
GEOPHYSICAL RESEARCH LETTERS, 2011, 38
[4]   Uncertainty analysis for estimates of the first indirect aerosol effect [J].
Chen, Y ;
Penner, JE .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :2935-2948
[5]  
Cooper W. A., 1988, Journal of Atmospheric and Oceanic Technology, V5, P823, DOI 10.1175/1520-0426(1988)005<0823:EOCOMW>2.0.CO
[6]  
2
[7]  
Dong X., 2010, J GEOPHYS RES, V115
[8]  
Dong XQ, 2002, J ATMOS SCI, V59, P3265, DOI 10.1175/1520-0469(2002)059<3265:COSCPD>2.0.CO
[9]  
2
[10]   First measurements of the Twomey indirect effect using ground-based remote sensors [J].
Feingold, G ;
Eberhard, WL ;
Veron, DE ;
Previdi, M .
GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (06) :20-1