Aerosol optical properties and their radiative effects in northern China
| Autor: | Zhanqing Li, Pucai Wang, Xiangao Xia, Si-Chee Tsay, Ellsworth G. Dutton, Fengsheng Zhao, Maureen Cribb, R. E. Dickerson, Wen Mi, Brent N. Holben, Hongbin Chen, Thomas F. Eck |
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| Rok vydání: | 2007 |
| Předmět: |
Atmospheric Science
Haze Ecology Meteorology Single-scattering albedo Paleontology Soil Science Forestry Aquatic Science Albedo Oceanography Atmospheric sciences complex mixtures Aerosol Atmosphere Troposphere Geophysics Space and Planetary Science Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) Atmospheric instability Radiative transfer Environmental science Earth-Surface Processes Water Science and Technology |
| Zdroj: | Journal of Geophysical Research. 112 |
| ISSN: | 0148-0227 |
| Popis: | [1] As a fast developing country covering a large territory, China is experiencing rapid environmental changes. High concentrations of aerosols with diverse properties are emitted in the region, providing a unique opportunity for understanding the impact of environmental changes on climate. Until very recently, few observational studies were conducted in the source regions. The East Asian Study of Tropospheric Aerosols: An International Regional Experiment (EAST-AIRE) attempts to characterize the physical, optical and chemical properties of the aerosols and their effects on climate over China. This study presents some preliminary results using continuous high-quality measurements of aerosol, cloud and radiative quantities made at the first EAST-AIRE baseline station at Xianghe, about 70 km east of Beijing over a period of one year (September 2004 to September 2005). It was found that the region is often covered by a thick layer of haze (with a yearly mean aerosol optical depth equal to 0.82 at 500 nm and maximum greater than 4) due primarily to anthropogenic emissions. An abrupt ‘‘cleanup’’ of the haze often took place in a matter of one day or less because of the passage of cold fronts. The mean single scattering albedo is approximately 0.9 but has strong day-to-day variations with maximum monthly averages occurring during the summer. Large aerosol loading and strong absorption lead to a very large aerosol radiative effect at the surface (the annual 24-hour mean values equals 24 W m � 2 ), but a much smaller aerosol radiative effect at the top of the atmosphere (one tenth of the surface value). The boundary atmosphere is thus heated dramatically during the daytime, which may affect atmospheric stability and cloud formation. In comparison, the cloud radiative effect at the surface is only moderately higher (� 41 W m � 2 ) than the aerosol radiative effect at the surface. |
| Databáze: | OpenAIRE |
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