Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.atmosenv.2019.06.027 |
Aerosol clustering in an urban environment of Beijing during (2005-2017) | |
Shaheen, Kausar1,2,3,4; Shah, Zarbad5; Suo, HongLi1,2; Liu, Min1,2; Ma, Lin1,2; Alam, Khan3; Gul, Alia6; Cui, Jin1,2; Li, Chunyan1,2; Wang, Ya1,2; Khan, Shahid Ali7; Khan, Sher Bahadar8,9 | |
通讯作者 | Shah, Zarbad |
来源期刊 | ATMOSPHERIC ENVIRONMENT
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ISSN | 1352-2310 |
EISSN | 1873-2844 |
出版年 | 2019 |
卷号 | 213页码:534-547 |
英文摘要 | In depth and detailed study about various classes of aerosols over an urban city of Beijing has been carried out, with the help of cluster technique during the period from (2005-2017). Aerosol Robotic Network (AERONET), retrieved data for Aerosol Optical Depth (AOD), Angstrom Exponent (AE), Extinction Angstrom Exponent (EAE), Absorption Angstrom Exponent (AAE), Single Scattering Albedo (SSA), Real and Imaginary index of Refraction (RRI & IRI respectively), Asymmetry Parameter (ASY) has been utilized for discrimination of aerosols over the study site. Higher mean values of AOD and AE were found in winter and spring season as (0.86 +/- 0.38, 0.85 +/- 0.32) and (1.06 +/- 0.36, 1.19 +/- 0.21), while lower values (0.75 +/- 0.33, 0.75 +/- 0.33) and (0.97 +/- 0.22, 0.85 +/- 0.17) for summer and autumn season respectively, representing mixed anthropogenic aerosols over the site. Three main types of aerosol were reported in this study: Mixed Carbonaceous (MC), Biomass Residuals (BR), and coarse mode local and transported Dust Particles (DP). Various aerosol parameters and their inter-relationship were investigated in detail to analyze the dominant aerosol type and its seasonal variations. The EAE and AAE values ranged from (0.10-1.77 and 0.00-1.70 respectively), could mainly be attributed towards MC aerosols. Real and Imaginary parts of Index (RRI & IRI) were recorded in the range from (1.33-1.60 and 0-0.010) respectively. Similarly, the range for SSA and ASY was found as (0.79-0.99 and 0.43-0.78) respectively. Back-trajectories using Hybrid Single Particle Lagrangian Integrated Trajectory (HYSPLIT) model revealed transportation of air masses from Mongolian deserts, Gobi desert, and other neighboring regions (i.e. Russia and Kazakhstan). |
英文关键词 | AERONET Aerosol optical depth Angstrom exponent Single scattering albedo Refractive index Asymmetry parameter |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China ; Pakistan ; Saudi Arabia |
收录类别 | SCI-E |
WOS记录号 | WOS:000484870900051 |
WOS关键词 | GROUND-BASED MEASUREMENTS ; INDO-GANGETIC PLAINS ; PEARL RIVER-DELTA ; OPTICAL-PROPERTIES ; SOURCE APPORTIONMENT ; PARTICULATE MATTER ; PARTICLE FORMATION ; 4 LOCATIONS ; HAZE EVENT ; AERONET |
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/2XILL650/214503 |
作者单位 | 1.Beijing Univ Technol, Key Lab Adv Funct Mat, Minist Educ, Beijing 100124, Peoples R China; 2.Beijing Univ Technol, Coll Mat Sci & Engn, Beijing 100124, Peoples R China; 3.Univ Peshawar, Dept Phys, Peshawar, Khyber Pakhtunk, Pakistan; 4.Univ Peshawar, Jinnah Coll Women, Dept Phys, Peshawar, Khyber Pakhtunk, Pakistan; 5.Bacha Khan Univ, Dept Chem, Charsadda, Khyber Pakhtunk, Pakistan; 6.Hazara Univ, Dept Bot, Mansehra, Khyber Pakhtunk, Pakistan; 7.Univ Swabi, Dept Chem, Anbar 23561, Khyber Pakhtunk, Pakistan; 8.King Abdulaziz Univ, Ctr Excellence Adv Mat Res, POB 80203, Jeddah 21589, Saudi Arabia; 9.King Abdulaziz Univ, Chem Dept, Fac Sci, POB 80203, Jeddah 21589, Saudi Arabia |
推荐引用方式 GB/T 7714 | Shaheen, Kausar,Shah, Zarbad,Suo, HongLi,et al. Aerosol clustering in an urban environment of Beijing during (2005-2017)[J],2019,213:534-547. |
APA | Shaheen, Kausar.,Shah, Zarbad.,Suo, HongLi.,Liu, Min.,Ma, Lin.,...&Khan, Sher Bahadar.(2019).Aerosol clustering in an urban environment of Beijing during (2005-2017).ATMOSPHERIC ENVIRONMENT,213,534-547. |
MLA | Shaheen, Kausar,et al."Aerosol clustering in an urban environment of Beijing during (2005-2017)".ATMOSPHERIC ENVIRONMENT 213(2019):534-547. |
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