地表反照率反演。
The results are helpful to improve the parameterization schemes of surface albedo in climate model and satellite remote sensing.
研究结果有助于改进气候模式和卫星遥感中高原地面反射率的参数化方案。
Wei Zhigang, Lü Shihua. 1995. Distribution of snow cover on the Qinghai-Xizang Plateau and its effect on surface albedo[J]. Plateau Meteor, 14(1):67-73.
韦志刚，吕世华.1995。青藏高原积雪的分布特征及其对地面反照率的影响[J]。高原气象，14（1）：67-73。
A model for the surface albedo responding to SWC and LAI was developed, which showed a good performance in consistent between simulated and observed surface albedo.
反映土壤含水量和叶面积指数共同作用的地表反射率模型的模拟值与野外实测值具有较好的一致性。
It shows how high surface albedo extends equatorwards in two opposing bulges into Asia and North America.
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。
The Role of Surface Albedo Feedback in Climate.
气候中地表反照率反馈影响。
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.
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。
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