气候中地表反照率反馈影响。
地表反照率反演。
本文的目的是对青藏高原地表反照率和冷热源参数进行定量反演。
The objective of this paper is to retrieve the albedo of the plateau and then to calculate the parameters about hot or cold source quantitatively.
它表明高的地表反照率如何在亚洲和北美两个相对的部位向着赤道扩展。
It shows how high surface albedo extends equatorwards in two opposing bulges into Asia and North America.
云和冰地表云对太阳辐射的传输：用光学厚度，太阳高度角和地表反照率参数化。
Transmission of Solar Radiation by Clouds over Snow and Ice Surfaces: a Parameterization in Terms of Optical Depth, Solar Zenith Angle, and Surface Albedo.
云和冰地表云对太阳辐射的传输：用光学厚度，太阳高度角和地表反照率参数化。
Transmission of Solar Radiation by Clouds over Snow and Ice Surfaces: a Parameterization in Terms of Optical Depth, Solar Zenith Angle, and Surface Albedo.
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