系列(地层学)
亮度
微波食品加热
盲信号分离
水分
亮度温度
环境科学
含水量
遥感
时间序列
数学
气象学
计算机科学
统计
地质学
物理
光学
电信
古生物学
频道(广播)
岩土工程
作者
Zebin Zhao,Rui Jin,Xin Li,Chunfeng Ma,Dazhi Li,Weizhen Wang,Zhongli Zhu
标识
DOI:10.1109/tgrs.2025.3573374
摘要
The effective use of observational constraints to mitigate the impacts of surface roughness and vegetation cover and the quantitative estimation of soil moisture from nonstationary microwave signals present critical challenges. Integrating the temporal constraints imposed by observations can provide additional information for achieving improved soil moisture estimation accuracy. Considering the time-dimensional autocorrelation of time-series passive microwave brightness temperatures, blind source separation (BSS) was introduced for soil moisture estimation. The single-channel BSS was used to decompose the brightness temperature into several intrinsic mode functions (IMFs). The Akaike information criterion and average silhouette width were used to recognize the number of blind sources based on the IMFs for multidimensional signal reconstruction. The multichannel BSS was carried out to decompose the reconstructed multidimensional signals to determine the trends of their blind sources to estimate soil moisture. An experiment conducted in Naqu demonstrated that the BSS-based method effectively estimated soil moisture, with an RMSE of 0.027 cm3/cm3. Through 1000 experiments, an error-bound analysis indicated that the method is robust, maintaining an average soil moisture estimation error of 0.032 cm3/cm3 [range 0–0.074 cm3/cm3]. Additionally, decomposing the SMAP brightness temperature for soil moisture estimation in Tianjun, Maqu, and Pali yielded good performance, with RMSEs of 0.037 cm3/cm3, 0.047 cm3/cm3, and 0.041 cm3/cm3, representing a significant improvement over the traditional inversion algorithms. Moreover, the proposed method bypasses the challenges of remote sensing-based soil moisture estimation, which is affected by variables such as surface roughness and vegetation cover. This changes the limitations of traditional soil moisture estimation methods that rely on microwave models.
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