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On Eastern Asian Dust Storm
引用本文:Zhao Bolin,Yu Xiaoding. On Eastern Asian Dust Storm[J]. 大气科学进展, 1990, 7(1): 11-26. DOI: 10.1007/BF02919164
作者姓名:Zhao Bolin  Yu Xiaoding
作者单位:Department of Geophysics,Peking University,Beijing 100871,Department of Geophysics,Peking University,Beijing 100871
摘    要:In this paper, the characteristics of eastern Asian dust storm are examined with emphasis on the satellite measurements of aerosol optical thickness. The reflectivity of solar radiation from the earth’s atmosphere depends on the optical thickness. The satellite measurement of radiance of sunlight, scattered by the earth and its atmosphere, is used to derive the properties of aerosol on oceanic surfaces. This paper involves the following: (1) investigation of the measurement of dust storm over the oceanic surface by GMS satellite; (2) investigation of the measurement of dust storm over the land surface by ground-based instruments such as actinometer, lidar, etc.; (3) for comparison, de-riving an atmospheric aerosol size distribution over the oceanic surface of calm weather through measurements of NOAA satellite; and (4) the weather process and its mass load of eastern Asian dust storm.


On eastern Asian dust storm
Zhao Bolin,Yu Xiaoding. On eastern Asian dust storm[J]. Advances in Atmospheric Sciences, 1990, 7(1): 11-26. DOI: 10.1007/BF02919164
Authors:Zhao Bolin  Yu Xiaoding
Affiliation:Department of Geophysics, Peking University, Beijing 100871,Department of Geophysics, Peking University, Beijing 100871
Abstract:In this paper, the characteristics of eastern Asian dust storm are examined with emphasis on the satellite measurements of aerosol optical thickness. The reflectivity of solar radiation from the earth's atmosphere depends on the optical thickness. The satellite measurement of radiance of sunlight, scattered by the earth and its atmosphere, is used to derive the properties of aerosol on oceanic surfaces. This paper involves the following: (1) investigation of the measurement of dust storm over the oceanic surface by GMS satellite; (2) investigation of the measurement of dust storm over the land surface by ground—based instruments such as actinometer, lidar, etc.; (3) for comparison, deriving an atmospheric aerosol size distribution over the oceanic surface of calm weather through measurements of NOAA satellite; and (4) the weather process and its mass load of eastern Asian dust storm.
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