GREENHOUSE IMPACTS OF ANTHROPOGENIC CH4 AND N2O EMISSIONS IN FINLAND

Citation
R. Pipatti et al., GREENHOUSE IMPACTS OF ANTHROPOGENIC CH4 AND N2O EMISSIONS IN FINLAND, Environmental management, 20(2), 1996, pp. 219-233
Citations number
44
Categorie Soggetti
Environmental Sciences
Journal title
ISSN journal
0364152X
Volume
20
Issue
2
Year of publication
1996
Pages
219 - 233
Database
ISI
SICI code
0364-152X(1996)20:2<219:GIOACA>2.0.ZU;2-7
Abstract
The Finnish anthropogenic CH, emissions in 1990 are estimated to be ab out 250 Gg, with an uncertainty range extending from 160 to 440 Gg. Th e mast important sources are landfills and animal husbandry. The N2O e missions, which come mainly from agriculture and the nitric acid indus try are about 20 Gg in 1990 (uncertainty range 10-30 Gg). The developm ent of the emissions to the year 2010 is reviewed in two scenarios: th e base and the reduction scenarios. According to the base scenario, th e Finnish CH, emissions will decrease in the near future. Emissions fr om landfills, energy production, and transportation will decrease beca use of already decided and partly realized volume and technical change s in these sectors. The average reduction potential of 50%, as assumed in the reduction scenario, is considered achievable. N2O emissions, o n the other hand, are expected to increase as emissions from energy pr oduction and transportation will grow due to an increasing use of flui dized bed boilers and catalytic converters in cars. The average reduct ion potential of 50%, as assumed in the reduction scenario, is optimis tic. Anthropogenic CH4 and N2O emissions presently cause about 30% of the direct radiative forcing due to Finnish anthropogenic greenhouse g as emissions. This share would be even larger if the indirect impacts of CH4 were included. The contribution of CH4 can be controlled due to its relatively short atmospheric lifetime and due to the existing emi ssion reduction potential. Nitrous oxide has a long atmospheric lifeti me and its emission control possiblities are limited; consequently, th e greenhouse impact of N2O seems to be increasing even if the emission s were limited somehow.