利用卫星资料估算沙漠地区黄沙尘云的光学参数

T. Kusaka, S. Mori, T. Suzuki, H. Shibata
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引用次数: 5

摘要

从中国北部沙漠运来的黄沙(日文称“沙”)经常在冬末和春季覆盖东亚。东亚地区大气中的尘埃粒子被认为是大气气溶胶的主要来源。本文提出了一种利用ADEOS/POLDER数据估算大气中黄沙尘光学特性和地面反射率的新算法。首先,由于在POLDER数据中难以识别广泛分布的雾霾云,通过模拟黄沙尘的远距离传输来估计黄沙尘的传输路径和全球质量分布;接下来,利用POLDER图像中选取的多个点在443 nm和670 nm波长处的多视点反射率和偏振,估算了沙漠地区朦胧科萨云的光学特性和地面反射率。结果表明,黄沙尘的折射率在1.45 ~ 1.55之间,黄沙尘的光学厚度t(443 nm)为0.42 ~ 0.47,在443 nm通道的地面反射率为0.09 ~ 0.15,在670 nm通道的地面反射率为0.28 ~ 0.31。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of optical parameters of yellow sand dust clouds over desert areas from satellite-level data
The yellow sand dust (called "kosa" in Japanese) transported from the deserts in the northern part of China often covers over East Asia in the late winter and spring. The dust particles in the atmosphere are regarded as a main source of atmospheric aerosols in East Asia. In this study, a new algorithm for estimating the optical properties of yellow sand dusts in the atmosphere and ground reflectances from ADEOS/POLDER data is described. First, the long-range transport of yellow sand dust was simulated to estimate the transport paths and the global mass distribution of yellow sand dust, because it is difficult to identify the widely spread hazy kosa cloud from POLDER data. Next, the optical properties of hazy kosa clouds over the desert area and ground reflectances were estimated, using the multi-viewing reflectances and polarizations at wavelengths 443 nm and 670 nm in several points selected from the POLDER image. As a result, it is shown that the refractive index of yellow sand dust is in the range from 1.45 to 1.55, and the optical thickness of yellow sand dust, t(443 nm) is 0.42 to 0.47, ground reflectance of the desert is 0.09 to 0.15 at the 443 nm channel, 0.28 to 0.31 at the 670 nm channel.
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