Impacts of increased anthropogenic emissions in Asia on tropospheric ozone and climate - A global 3-D model study

被引:77
作者
Berntsen, T
Isaksen, ISA
Wang, WC
Liang, XZ
机构
[1] UNIV OSLO,CTR INT CLIMATE & ENVIRONM RES,N-0317 OSLO,NORWAY
[2] SUNY ALBANY,ATMOSPHER SCI RES CTR,ALBANY,NY 12222
关键词
D O I
10.1034/j.1600-0889.1996.00003.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A global 3-dimensional chemical transport model (CTM) has been used to study the impact of enhanced emission of pollutants in the Asian region on key chemical species like O-3, OH and nitrogen oxides. An extended set of chemical compounds are included in the model, of which 25 are transported. Diurnal variations are calculated, including the diurnal cycle of photodissociation rates. The Asian region has been selected for this perturbation study since emissions are rapidly increasing in this region, and because there is a large potential for Future increases. A 15-month reference run and 2 perturbation studies, both starling in May and running for 4 months are performed, one with increases in NOx emission of a factor of 2 and one with a factor 4. Increases in the anthropogenic emissions of hydrocarbons and CO are also included. Results for the last month (August) are then compared with the results from the reference run for the same month. In the 3-D model calculations, the adopted perturbations lead to significant increases in surface ozone in the Asian region. It is interesting to notice that enhanced short term ozone values during episodes are becoming more pronounced in the cases with high emissions. Significant ozone increases are also obtained in the upper troposphere due to efficient convective transport. The impact is noticible over a larger region in the free troposphere than in the surface layer due to longer chemical lifetime of ozone, and an efficient transport. A doubling of NOx emission, gives significant ozone increases up to 30 % in the upper troposphere. Calculations of the regionally positive radiative forcing from the increases in tropospheric ozone show values of about 0.5 W/m(2), which is 30-50 % of the estimated negative radiative forcing due to the direct effect of sulphate aerosols in the region.
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页码:13 / 32
页数:20
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