Observations of Black Carbon characteristics and radiative forcing over a Global Atmosphere Watch supersite in Korea

被引:23
|
作者
Panicker, A. S. [1 ]
Park, Sung-Hwa [2 ]
Lee, Dong-In [2 ]
Kim, Dong-Chul [3 ,4 ]
Jung, Woon-Seon [2 ]
Jang, Sang-Min [2 ]
Jeong, Jong-Hoon [2 ]
Kim, Dong-Soon [5 ]
Yu, Jegyu [6 ]
Jeong, Harrison [6 ]
机构
[1] Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India
[2] Pukyong Natl Univ, Dept Environm Atmospher Sci, Atmospher Environm Res Inst, Pusan, South Korea
[3] Univ Maryland Baltimore Cty, Goddard Earth Sci & Technol Ctr, Baltimore, MD 21228 USA
[4] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[5] Natl Res Inst Earth Sci & Disaster Prevent, Tsukuba, Ibaraki, Japan
[6] Korea Meteorol Adm, Korea Global Atmosphere Watch Ctr, Seoul, South Korea
基金
新加坡国家研究基金会;
关键词
Black carbon; Aerosol optical depth; Radiative forcing; OPTICAL-PROPERTIES; AEROSOLS; TRANSPORT; AREA;
D O I
10.1016/j.atmosenv.2013.04.020
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper provides an account of observed variations in Black carbon (BC) mass concentrations and BC induced radiative forcing for the first time over a background Global Atmosphere Watch (GAW) site, Anmyeon in South Korea. BC concentrations were continuously measured over the site during January 2003-December 2004 periods using an Aethalometer. BC showed higher concentrations during 2003 in majority of the months (except in January, August and October). BC found to be showing higher concentrations in September 2003, with values reaching up to 3 mu g m(-3) over the site. It also showed higher peaks in May and December in 2003. BC values were found to be comparatively less during wet season (July-August; especially august), which could be associated with the rainout and washout associated with the Changma season (summer monsoon). Optical Properties of Aerosols and Clouds (OPAC) model in combination with a radiative transfer model (SBDART) were used to estimate aerosol radiative forcing separately for composite aerosols (total aerosols) and solely for BC aerosols using chemical composition data sets of Total Suspended Particulates (TSP) and BC. The atmospheric forcing for composite aerosols found to be +14.9 to +25.9 W m(-2) during spring, +13.4 to +20.4 W m(-2) in summer, +12.9 to +19.1 W m(-2) in autumn and +16 to +18.2 W m(-2) during winter, respectively. The respective BC atmospheric forcings were +8.1 to +11.8 W m(-2), +8.4 to +11.1 W m(-2), +8.7 to +11.4 W m(-2) and +8.8 to +11.7 W m(-2) during spring, summer, autumn and winter. The study suggests that BC induced atmospheric forcing can contribute up to 88% of total aerosol induced atmospheric warming. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:98 / 104
页数:7
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