The Relationship Between the Variation Rate of MODIS Land Surface Temperature and AMSR-E Soil Moisture and Its Application to Downscaling

被引:0
|
作者
Wang An-qi [1 ,2 ]
Xie Chao [3 ]
Shi Jian-cheng [2 ]
Gong Hui-li [1 ]
机构
[1] Capital Normal Univ, Base State Lab Urban Environm Proc & Digital Mode, Beijing 100048, Peoples R China
[2] Chinese Acad Sci, Inst Remote Sensing Applicat, Beijing 100101, Peoples R China
[3] Peking Univ, Inst Remote Sensing & GIS, Beijing 100871, Peoples R China
关键词
Passive microwave; Soil moisture; Land surface temperature; Instantaneous variation; Power exponent function; Downscaling;
D O I
10.3964/j.issn.1000-0593(2013)03-0623-05
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
Using AMSR-E soil moisture, MODIS land surface temperature (T-s) and vegetation index product, the authors discuss the relationship between the variation rate of land surface temperature and surface soil moisture. Selecting the plains region of central United States as the study area, the authors propose the distribution triangle of the variation rate of land surface temperature and soil moisture. In the present paper, temperature variation and vegetation index (TVVI), a new index containing the information of temperature variation and vegetation, is introduced. The authors prove that TVVI and soil moisture show a steady relationship of exponential function; and build a quantitative model of soil moisture(SM) and instantaneous surface temperature variation (V-Ts). The authors later achieve downscaling of AMSR-E soil moisture data, through the above stated functional relationships and high-resolution MODIS data. Comparison with measured data on ground surface indicates that this method of downscaling is of high precision.
引用
收藏
页码:623 / 627
页数:5
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