《Table 2 Soil moisture of major soil types in Qinghai Lake Basin, China (early October 2016)》
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《Remotely sensed estimation and mapping of soil moisture by eliminating the effect of vegetation cover》
The errors between estimated SM from the two models and the actual measured SM data were analyzed(Table 1).For all samples except C04-1,D11-1,and A10-1,the AE and RE of the bare soil albedo model were smaller than those of the surface albedo model.The model errors increased rapidly when SM was less than 10.0%.In addition,the RMSE,MAPE and TIC of the bare soil albedo model were smaller than those of the surface albedo model.
图表编号 | XD0047431400 严禁用于非法目的 |
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绘制时间 | 2019.02.20 |
作者 | WU Cheng-yong、CAO Guang-chao、CHEN Ke-long、E Chong-yi、MAO Ya-hui、ZHAO Shuang-kai、WANG Qi、SU Xiao-yi、WEI Ya-lan |
绘制单位 | College of Geographical Sciences, Qinghai Normal University、Key Laboratory of Environment and Ecology of Qinghai-Tibet Plateau, Ministry of Education、Qinghai Key Laboratory of Natural Geography and Environmental Processes、Key Laboratory of Environment and |
更多格式 | 高清、无水印(增值服务) |
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