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Estimating the spatial distribution of soil moisture based on Bayesian maximum entropy method with auxiliary data from remote sensing

机译:基于贝叶斯最大熵法的遥感辅助数据估算土壤水分的空间分布

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摘要

Soil moisture (SM) plays a fundamental role in the land-atmosphere exchange process. Spatial estimation based on multi in situ (network) data is a critical way to understand the spatial structure and variation of land surface soil moisture. Theoretically, integrating densely sampled auxiliary data spatially correlated with soil moisture into the procedure of spatial estimation can improve its accuracy. In this study, we present a novel approach to estimate the spatial pattern of soil moisture by using the BME method based on wireless sensor network data and auxiliary information from ASTER (Terra) land surface temperature measurements. For comparison, three traditional geostatistic methods were also applied: ordinary kriging (OK), which used the wireless sensor network data only, regression kriging (RK) and ordinary co-kriging (Co-OK) which both integrated the ASTER land surface temperature as a covariate. In Co-OK, LST was linearly contained in the estimator, in RK, estimator is expressed as the sum of the regression estimate and the kriged estimate of the spatially correlated residual, but in BME, the ASTER land surface temperature was first retrieved as soil moisture based on the linear regression, then, the t-distributed prediction interval (PI) of soil moisture was estimated and used as soft data in probability form. The results indicate that all three methods provide reasonable estimations. Co-OK, RK and BME can provide a more accurate spatial estimation by integrating the auxiliary information Compared to OK. RK and BME shows more obvious improvement compared to Co-OK, and even BME can perform slightly better than RK. The inherent issue of spatial estimation (overestimation in the range of low values and underestimation in the range of high values) can also be further improved in both RK and BME. We can conclude that integrating auxiliary data into spatial estimation can indeed improve the accuracy, BME and RK take better advantage of the auxiliary information compared to Co-OK, and BME outperforms RK by integrating the auxiliary data in a probability form.
机译:土壤水分(SM)在陆地-大气交换过程中起着基本作用。基于多原位(网络)数据的空间估计是了解土地表层土壤水分的空间结构和变化的关键方法。从理论上讲,将与土壤水分在空间上相关的密集采样辅助数据整合到空间估计过程中可以提高其准确性。在这项研究中,我们提出了一种基于无线传感器网络数据和ASTER(Terra)地表温度测量的辅助信息,通过BME方法估算土壤水分空间格局的新方法。为了进行比较,还使用了三种传统的地统计方法:普通克里格法(OK)仅使用无线传感器网络数据;回归克里格法(RK)和普通协克里格(Co-OK)都将ASTER地表温度作为协变量在Co-OK中,LST线性包含在估算器中,在RK中,估算器表示为回归估计值与空间相关残差的kriged估计值之和,但在BME中,首先将ASTER地表温度作为土壤检索基于线性回归,计算土壤水分的t分布预测间隔(PI),并以概率形式将其用作软数据。结果表明,这三种方法均提供了合理的估计。与OK相比,Co-OK,RK和BME可以通过集成辅助信息来提供更准确的空间估计。与Co-OK相比,RK和BME的改进更为明显,甚至BME的性能也比RK稍好。在RK和BME中,空间估计的固有问题(低值范围内的高估和高值范围内的低估)也可以得到进一步改善。我们可以得出结论,将辅助数据集成到空间估计中确实可以提高准确性,与Co-OK相比,BME和RK更好地利用了辅助信息,并且BME通过以概率形式集成辅助数据胜过RK。

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