Characteristics of Chinese aerosols determined by individual‐particle analysis

Tropospheric aerosols that originate in China and are transported over the North Pacific Ocean have potentially significant impacts on regional and global climate. These aerosols are complex mixtures of soil dust and anthropogenic particles from a variety of sources, including fossil fuel combustion, biomass burning, mining, smelting, and other industrial processes, plus reaction products of heterogeneous processes that affect these particles during transport. In the coastal marine atmosphere, these particles could be further mixed with marine aerosols. To provide examples of the diversity of chemical and physical properties of east Asian aerosols in the spring, individual aerosol particle samples were collected in April and May 1999 in three different environments in China: Qingdao on the coast of the East China Sea, Beijing in the northeast interior, and Mount Waliguan in remote northwestern China. Results reveal that aerosols in this region are complex and heterogeneous. In addition to significant differences in aerosol composition and size distributions among the samples, each sample contains a large number of polyphase aggregates. Many of the particles also have irregular shapes; for a number of the particle types, the irregular shapes should persist even at high ambient RH. Because composition, degree and nature of polyphase aggregation, and shape all effect aerosol radiative properties, the complex state of east Asian aerosols presents a challenge for the modeling of aerosol radiative forcing in the region.

[1]  Nobuo Kato,et al.  Anthropogenic emissions of SO2 and NOx in Asia : emission inventories , 1992 .

[2]  Irina N. Sokolik,et al.  Incorporation of mineralogical composition into models of the radiative properties of mineral aerosol from UV to IR wavelengths , 1999 .

[3]  Min Hu,et al.  Mixture of sulfate and nitrate in coastal atmospheric aerosols: individual particle studies in Qingdao (36°04′N, 120°21′E), China , 2000 .

[4]  Peter R. Buseck,et al.  Characterization of individual fine-fraction particles from the Arctic aerosol at Spitsbergen, May–June 1987 , 1992 .

[5]  J. W. Winchester,et al.  Acid‐base balance in aerosol components of the Asia‐Pacific region , 1989 .

[6]  J. Coakley,et al.  Climate Forcing by Anthropogenic Aerosols , 1992, Science.

[7]  P. Buseck,et al.  Characterization of the Bermuda tropospheric aerosol by combined individual-particle and bulk-aerosol analysis , 1996 .

[8]  J. Prospero,et al.  Deposition of atmospheric mineral particles in the North Pacific Ocean , 1985 .

[9]  D Eastwood,et al.  Oil-matching by using a simple vector model for fluorescence spectra. , 1981, Talanta.

[10]  S. Taylor The continental crust , 1985 .

[11]  J. Penner,et al.  Quantifying and minimizing uncertainty of climate forcing by anthropogenic aerosols , 1994 .

[12]  P. Bhartia,et al.  Derivation of aerosol properties from satellite measurements of backscattered ultraviolet radiation , 1998 .

[13]  W. Chan,et al.  Acid rain in southwestern China , 1988 .

[14]  H. Ueda,et al.  Seasonal variation of aerosol composition at Cheju Island, Korea , 1996 .

[15]  R. Duce,et al.  Relationships between the dust concentrations over eastern Asia and the remote North Pacific , 1992 .

[16]  Akira Ono,et al.  Transport of Asian dust (KOSA) particles; importance of weak KOSA events on the geochemical cycle of soil particles , 1988 .

[17]  H. Naruse,et al.  X-ray spectrometry of individual Asian dust-storm particles over the Japanese islands and the North Pacific Ocean , 1990 .

[18]  A. Lacis,et al.  The influence on climate forcing of mineral aerosols from disturbed soils , 1996, Nature.

[19]  Xiaoye Zhang,et al.  Temporal and spatial distributions of dust and its deposition to the China Sea , 1997 .

[20]  J. Lelieveld,et al.  Role of mineral aerosol as a reactive surface in the global troposphere , 1996 .

[21]  Irina N. Sokolik,et al.  Direct radiative forcing by anthropogenic airborne mineral aerosols , 1996, Nature.

[22]  P. Buseck,et al.  Soot and sulfate aerosol particles in the remote marine troposphere , 1999 .

[23]  R. Duce,et al.  Input of atmospheric trace elements and mineral matter to the Yellow Sea during the spring of a low‐dust year , 1992 .

[24]  Itsushi Uno,et al.  Transport of Asian air pollution to North America , 1999 .

[25]  R. Sherrell,et al.  Direct determination of 10 trace metals in 50 µL samples of coastal seawater using desolvating micronebulization sector field ICP-MS , 1999 .

[26]  J. Prospero,et al.  Long-Range Atmospheric Transport of Soil Dust from Asia to the Tropical North Pacific: Temporal Variability , 1980, Science.

[27]  J D Lindberg,et al.  Ultraviolet and visible imaginary refractive index of strongly absorbing atmospheric particulate matter. , 1992, Applied optics.

[28]  Gregory R. Carmichael,et al.  Photochemical Oxidant Processes in the Presence of Dust: An Evaluation of the Impact of Dust on Particulate Nitrate and Ozone Formation , 1994 .

[29]  T. Nakajima,et al.  The coarse particle aerosols in the free troposphere around Japan , 1990 .