Anthropogenic sulphate aerosol from India: estimates of burden and direct radiative forcing

被引:26
作者
Venkataraman, C [1 ]
Chandramouli, B
Patwardhan, A
机构
[1] Indian Inst Technol, Ctr Environm Sci & Engn, Powai 400076, Mumbai, India
[2] Indian Inst Technol, Sch Management, Powai 400076, Mumbai, India
关键词
global climate; sulphate aerosol; India; anthropogenic SO(2) emissions; chemical-meteorological box model;
D O I
10.1016/S1352-2310(98)00140-X
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A one-box chemical-meteorological model had been formulated to make preliminary estimates of sulphate aerosol formation and direct radiative forcing over India. Anthropogenic SO(2) emissions from India, from industrial fuel use and biomass burning, were estimated at 2.0 Tg S yr(-1) for 1990 in the range of previous estimates of 1.54 and 2.55 Tg S yr(-1) for 1987. Meteorological parameters for 1990 from 18 Indian Meteorological Department stations were used to estimate spatial average sulphate burdens through formation from SO(2) reactions in gas and aqueous phase and removal by dry and wet deposition. The hydrogen peroxide reaction was found dominating for undepleted oxidant-rich conditions. Monthly mean sulphate burdens ranged from 2-10 mg m(-2) with a seasonal variation of winter-spring highs and summer lows in agreement with previous GCM studies. The sulphate burdens are dominated by sulphate removal rates by wet deposition, which are high in the monsoon period from June-November. Monthly mean direct radiative forcing from sulphate aerosols is high (-3.5 and -2.3 W m(-2)) in December and January, is moderate (-1.3 to -1.5 W m(-2)) during February to April and November and low ( -0.4 to -0.6 W m(-2)) during May to October also in general agreement with previous GCM estimates. This model, in reasonable agreement with detailed GCM results, gives us a simple tool to make preliminary estimates of sulphate burdens and direct radiative forcing. (C) 1999 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:3225 / 3235
页数:11
相关论文
共 41 条
[1]   BIOMASS-BURNING EMISSIONS AND ASSOCIATED HAZE LAYERS OVER AMAZONIA [J].
ANDREAE, MO ;
BROWELL, EV ;
GARSTANG, M ;
GREGORY, GL ;
HARRISS, RC ;
HILL, GF ;
JACOB, DJ ;
PEREIRA, MC ;
SACHSE, GW ;
SETZER, AW ;
DIAS, PLS ;
TALBOT, RW ;
TORRES, AL ;
WOFSY, SC .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1988, 93 (D2) :1509-1527
[2]  
[Anonymous], GREENHOUSE GAS EMISS
[3]   General circulation model assessment of the sensitivity of direct climate forcing by anthropogenic sulfate aerosols to aerosol size and chemistry [J].
Boucher, O ;
Anderson, TL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D12) :26117-26134
[4]  
BOUCHER O, 1997, COMMUNICATION
[5]   CLIMATE FORCING BY ANTHROPOGENIC AEROSOLS [J].
CHARLSON, RJ ;
SCHWARTZ, SE ;
HALES, JM ;
CESS, RD ;
COAKLEY, JA ;
HANSEN, JE ;
HOFMANN, DJ .
SCIENCE, 1992, 255 (5043) :423-430
[6]  
CHARLSON RJ, 1991, TELLUS A, V43, P152, DOI 10.1034/j.1600-0870.1991.00013.x
[7]   Anthropogenic and natural contributions to tropospheric sulfate: A global model analysis [J].
Chin, M ;
Jacob, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D13) :18691-18699
[8]   A global three-dimensional model of tropospheric sulfate [J].
Chin, M ;
Jacob, DJ ;
Gardner, GM ;
ForemanFowler, MS ;
Spiro, PA ;
Savoie, DL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D13) :18667-18690
[9]  
CUKIER RL, 1973, J CHEM PHYS, V159, P3873
[10]   Simulation of the tropospheric sulfur cycle in a global climate model [J].
Feichter, J ;
Kjellstrom, E ;
Rodhe, H ;
Dentener, F ;
Lelieveld, J ;
Roelofs, GJ .
ATMOSPHERIC ENVIRONMENT, 1996, 30 (10-11) :1693-1707