Dynamic Distribution and Albedo Change of Snow in China
中国地表积雪动态分布及反照率的变化

Different land surface feature and physical characteristics cause anisotropy energy distribution. They influence on regional and global climate change because of snow wide distribution, high albedo and continuous seasonal change. Remote sensing which monitors the change of land surface feature and derives regional albedo is an effective measure. In this paper, we study dynamic distribution of snow and dynamic change of albedo through remote sensing technology.