Continuous observations of Asian dust and other aerosols by polarization lidars in China and Japan during ACE-Asia

[1] Continuous observations of aerosols in China and Japan were made by polarization lidars during March to May 2001, corresponding with the Asian Pacific Regional Aerosol Characterization Experiment (ACE-Asia) field campaign period. Lidars in Beijing, Nagasaki, and Tsukuba were continuously operated regardless of weather conditions. Scatterers in the atmosphere were categorized for all vertical profiles, and occurrence frequencies of dust, spherical aerosols, and clouds up to 6 km were calculated. The frequency of dust was highest in Beijing for the whole height range. There was a peak of dust occurrence near the ground in Nagasaki. Dust was frequently detected in the free troposphere in Tsukuba. The contributions of dust and spherical aerosols to the total backscattering coefficient were estimated from the depolarization ratio with the assumption of the external mixture of both kinds of aerosols. Vertical profiles of backscattering by dust and by spherical aerosols represented the different characteristics of these aerosols. The monthly averaged backscattering coefficients by dust near the surface were 0.003/km/sr in Beijing, 0.001–0.002/km/sr in Nagasaki, and 0.0006/km/sr in Tsukuba. The backscattering coefficients by spherical aerosols near the surface were 0.002–0.004/km/sr at all three observatories. We compared the derived backscattering coefficients with aerosol mass concentrations calculated by a numerical model, Chemical Weather Forecasting System (CFORS). CFORS reproduced well the vertical structures of the tall dust events and the enhancements of spherical aerosols throughout the observation period. A specific dust event on 16–19 May 2001 was analyzed by using five lidars in Japan, and its fine structure is described.

[1]  Teruyuki Nakajima,et al.  Observation of dust and anthropogenic aerosol plumes in the Northwest Pacific with a two‐wavelength polarization lidar on board the research vessel Mirai , 2002 .

[2]  Takashi Shibata,et al.  Free tropospheric aerosol backscatter, depolarization ratio, and relative humidity measured with the Raman lidar at Nagoya in 1994-1997: contributions of aerosols from the Asian Continent and the Pacific Ocean , 2000 .

[3]  H. Okamoto,et al.  Application of lidar depolarization measurement in the atmospheric boundary layer: Effects of dust and sea‐salt particles , 1999 .

[4]  Nobuo Sugimoto,et al.  Trans‐Pacific yellow sand transport observed in April 1998: A numerical simulation , 2001 .

[5]  F. G. Fernald Analysis of atmospheric lidar observations: some comments. , 1984, Applied optics.

[6]  Hiroaki Minoura,et al.  The transport and spacial scale of Asian dust‐storm clouds: a case study of the dust‐storm event of April 1979 , 1983 .

[7]  P. Koepke,et al.  Optical Properties of Aerosols and Clouds: The Software Package OPAC , 1998 .

[8]  N. S. Higdon,et al.  Airborne lidar observations in the wintertime Arctic stratosphere: Polar stratospheric clouds , 1990 .

[9]  G. Carmichael,et al.  Regional chemical weather forecasting system CFORS: Model descriptions and analysis of surface observations at Japanese island stations during the ACE‐Asia experiment , 2003 .

[10]  Albert Ansmann,et al.  Vertical profiling of optical and physical particle properties over the tropical Indian Ocean with six‐wavelength lidar: 2. Case studies , 2001 .

[11]  J. Heintzenberg Fine particles in the global troposphere. A review , 1989 .

[12]  Robert Frouin,et al.  Asian Dust Events of April 1998 , 2001 .

[13]  Gunnar Myhre,et al.  Global sensitivity experiments of the radiative forcing due to mineral aerosols , 2001 .

[14]  A. Ansmann,et al.  Dual‐wavelength Raman lidar observations of the extinction‐to‐backscatter ratio of Saharan dust , 2002 .

[15]  Kengo Iokibe,et al.  Ground‐based network observation of Asian dust events of April 1998 in east Asia , 2001 .

[16]  D. Tanré,et al.  Characterization of aerosol spatial distribution and optical properties over the Indian Ocean from airborne LIDAR and radiometry during INDOEX'99 , 2002 .

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

[18]  Philip B. Russell,et al.  Aerosol properties and radiative effects in the United States East Coast haze plume: An overview of the Tropospheric Aerosol Radiative Forcing Observational Experiment (TARFOX) , 1999 .

[19]  Zhaoyan Liu,et al.  Extinction-to-backscatter ratio of Asian dust observed with high-spectral-resolution lidar and Raman lidar. , 2002, Applied optics.

[20]  Glenn E. Shaw,et al.  Indian Ocean Experiment: An integrated analysis of the climate forcing and effects of the great Indo-Asian haze , 2001 .