Radiative Forcing of SO2 and NOx: A Case Study in Beijing

A case study was performed in Beijing in 2000 to observe concentrations of SO2 and NOx in the atmosphere and to evaluate their radiative impact. It was found that the concentrations of these gases are usually high in the morning due to a temperature inversion in the boundary layer. The average conce...

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Published inAdvances in atmospheric sciences Vol. 23; no. 2; pp. 317 - 322
Main Author 孙治安 王晓云 曾宪宁
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Nature B.V 01.03.2006
Bureau of Meteorology Research Centre, GPO BOX 1289K, Melbourne 3001, Australia%Beijing Regional Meteorological Centre, Beijing%Nanjing University of Information Science and Technology,Nanjing,210044
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ISSN0256-1530
1861-9533
DOI10.1007/s00376-006-0317-6

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Summary:A case study was performed in Beijing in 2000 to observe concentrations of SO2 and NOx in the atmosphere and to evaluate their radiative impact. It was found that the concentrations of these gases are usually high in the morning due to a temperature inversion in the boundary layer. The average concentrations obtained from the observations are much higher than those used in the McClatchey reference atmosphere. The radiative impacts of these gases are calculated using a line-by-line radiative transfer model. The results show that the radiative forcing at the surface due to SO2 is 0.0576 W m^-2 and that due to NOx is 0.0032 W m^-2. These figures are almost compatible with that due to CFC11.
Bibliography:air pollution, radiative forcing, gas concentration, greenhouse effect
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ISSN:0256-1530
1861-9533
DOI:10.1007/s00376-006-0317-6