Arid
DOI10.1016/j.atmosenv.2010.07.043
Aerosol optical properties of regional background atmosphere in Northeast China
Wang, Peng2; Che, Huizheng1; Zhang, Xiaochun1; Song, Qingli2; Wang, Yaqiang1; Zhang, Zhonghua2; Dai, Xin2; Yu, Dajiang2
通讯作者Che, Huizheng
来源期刊ATMOSPHERIC ENVIRONMENT
ISSN1352-2310
EISSN1873-2844
出版年2010
卷号44期号:35页码:4404-4412
英文摘要

Aerosol optical properties from 2005 to 2008 at the Longfengshan regional background station in Northeast China were measured and analyzed. The annual mean of aerosol optical depth (AOD) at 440 nm for the four years was about 0.27 +/- 0.25, 0.39 +/- 0.37, 0.35 +/- 0.34, and 0.38 +/- 0.38, respectively, and the corresponding annual mean for the Angstrom exponent between 440 nm and 870 nm was about 1.43 +/- 0.48, 1.23 +/- 0.37, 1.53 +/- 0.47, and 1.55 +/- 0.42. The average monthly AOD(440nm) showed similar seasonal variation with a maximum in spring and a minimum in autumn. The monthly means of AOD at 440, 675, 870 and 1020 nm increase from the January to March with the maxima about 0.77 +/- 0.04, 0.65 +/- 0.04, 0.58 +/- 0.06, 0.57 +/- 0.07. respectively and decrease from September to February with the minima about 0.32 +/- 0.12, 0.22 +/- 0.09, 0.15 +/- 0.08, and 0.13 +/- 0.07 in January. The monthly mean of Angstrom exponent shows a minimum in March (0.97 +/- 0.52) and a maximum in September (1.66 +/- 0.29). Both the AOD and Angstrom exponent presents single peak distributions of occurrence frequencies. The Longfenshan data showed high AODs (>1.00) both clustering in the fine mode growth wing and the coarse mode. Two typical cases under dust and haze conditions showed that the AOD under dusty day decreased from 2.20 to 1.20 and the Angstrom exponent increased from 0.10 to 1.00. On the contrast, the AOD under haze day remained relatively stable about 0.90 and the Angstrom exponent was around 1.40. The 3-day backtrajectory analysis at Longfengshan illustrated that the air-masses near ground on the dust day were from Bohai Sea and passed through Liaodong Peninsula and Northeast plain in China. But the air-masses on 500 m AGL were originated from western Mongolia and crossed Gobi deserts, Otindag Sand Land and Horqin Sand Land in Northeast China. The air-masses at Longfengshan near ground 500 m and 1000 m AGL on the haze days were from North China Region and passed through Northeast Heavy Industrial Base in Northeast China. Crown Copyright (C) 2010 Published by Elsevier Ltd. All rights reserved.


英文关键词Aerosol optical depth Angstrom exponent Longfengshan background station Backtrajectory analysis China
类型Article
语种英语
国家Peoples R China
收录类别SCI-E
WOS记录号WOS:000283568300010
WOS关键词AERONET ; NETWORK ; SUN ; SATELLITE ; DEPTH ; DUST
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/163365
作者单位1.CMA, Chinese Acad Meteorol Sci, Ctr Atmosphere Watch & Serv, Key Lab Atmospher Chem, Beijing 100081, Peoples R China;
2.Heilongjiang Meteorol Adm, Longfengshan Atmospher Background Reg Stn, Wuchang 150209, Heilongjiang, Peoples R China
推荐引用方式
GB/T 7714
Wang, Peng,Che, Huizheng,Zhang, Xiaochun,et al. Aerosol optical properties of regional background atmosphere in Northeast China[J],2010,44(35):4404-4412.
APA Wang, Peng.,Che, Huizheng.,Zhang, Xiaochun.,Song, Qingli.,Wang, Yaqiang.,...&Yu, Dajiang.(2010).Aerosol optical properties of regional background atmosphere in Northeast China.ATMOSPHERIC ENVIRONMENT,44(35),4404-4412.
MLA Wang, Peng,et al."Aerosol optical properties of regional background atmosphere in Northeast China".ATMOSPHERIC ENVIRONMENT 44.35(2010):4404-4412.
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