Aircraft study of aerosol vertical distributions over Beijing and their optical properties

被引:117
作者
Liu, Pengfei [1 ]
Zhao, Chunsheng [1 ]
Zhang, Qiang [2 ]
Deng, Zhaoze [1 ]
Huang, Mengyu [1 ,2 ]
Ma, Xincheng [2 ]
Tie, Xuexi [3 ]
机构
[1] Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China
[2] Beijing Meteorol Bur, Beijing Weather Modificat Off, Beijing, Peoples R China
[3] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
基金
中国国家自然科学基金;
关键词
IN-SITU; SIZE DISTRIBUTIONS; DUST; POLLUTION; CLOSURE; CLOUDS;
D O I
10.1111/j.1600-0889.2009.00440.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A set of 152 vertical profiles of aerosol number concentration and size distribution with diameter ranging from 0.12 to 3.0 mu m observed by the airborne optical spectrometer probe in Beijing, China, between February 2005 and September 2006 is analysed and discussed. The statistic of aerosol number concentration (N-a) reveals a high aerosol number density in this region with average surface level number concentration (N-0) of about 6600 cm-3 (0.12-3.0 mu m). The average vertical profile of N-a approximately satisfies an exponential decline function with a scale height of 1419 m. The N-a profiles are influenced by the structures of planetary boundary layer (PBL) significantly and two typical types of N-a profile under different conditions of PBL are presented and parametrized in this study. The observations of aerosol size distribution show that, in most cases the aerosol size distributions are not very sensitive to altitude, with effective radii ranging from 0.16 to 0.28 mu m. Comparison between aircraft-derived aerosol optical depth (AOD) and Moderate Resolution Imaging Spectroradiometer-derived AOD shows good agreement. The Mie model calculations suggest that the surface level number concentration, the PBL height and the structure of PBL can influence the AOD significantly.
引用
收藏
页码:756 / 767
页数:12
相关论文
共 31 条
[11]   Statistical analysis of microphysical properties and the parameterization of effective radius of warm clouds in Beijing area [J].
Deng, Zhaoze ;
Zhao, Chunsheng ;
Zhang, Qiang ;
Huang, Mengyu ;
Ma, Xincheng .
ATMOSPHERIC RESEARCH, 2009, 93 (04) :888-896
[12]  
Draxler R.R., 2003, HYSPLIT HYBRID SINGL, DOI DOI 10.1175/BAMS-D-14-00110.1
[13]   The vertical distribution of aerosols, Saharan dust and cirrus clouds in Rome (Italy) in the year 2001 [J].
Gobbi, GP ;
Barnaba, F ;
Ammannato, L .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2004, 4 :351-359
[14]   Long range trans-Pacific transport and deposition of Asian dust aerosols [J].
Han Yongxiang ;
Fang Xiaomin ;
Zhao Tianliang ;
Kang Shichang .
JOURNAL OF ENVIRONMENTAL SCIENCES, 2008, 20 (04) :424-428
[15]   Airborne measurements of aerosol extinction in the lower and middle troposphere over Wyoming, USA [J].
Han, ZG ;
Montague, DC ;
Snider, JR .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (06) :789-802
[16]   Comparison of aerosol size distributions, radiative properties, and optical depths determined by aircraft observations and Sun photometers during SAFARI 2000 [J].
Haywood, J ;
Francis, P ;
Dubovik, O ;
Glew, M ;
Holben, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D13)
[17]   Recent frequent dust events and their relation to surface wind in East Asia [J].
Kurosaki, Y ;
Mikami, M .
GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (14) :ASC2-1
[18]  
LI C, 2003, CHINESE SCI BULL, V28, P2488
[19]  
Rolph G.D., 2003, REAL TIME ENV APPL D
[20]   Clear-sky closure studies of lower tropospheric aerosol and water vapor during ACE-2 using airborne sunphotometer, airborne in-situ, space-borne, and ground-based measurements [J].
Schmid, B ;
Livingston, JM ;
Russell, PB ;
Durkee, PA ;
Jonsson, HH ;
Collins, DR ;
Flagan, RC ;
Seinfeld, JH ;
Gassó, S ;
Hegg, DA ;
Öström, E ;
Noone, KJ ;
Welton, EJ ;
Voss, KJ ;
Gordon, HR ;
Formenti, P ;
Andreae, MO .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02) :568-593