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A new non-parametric Bayesian based space upscaling method for in-situ soil moisture sampling

机译:一种新的基于非贝叶斯贝叶斯空间放大的原位土壤水分采样方法

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In soil moisture remote sensing products ground verification, the soil moisture in-situ sampling is heterogeneous and not consistent with the remote sensing pixel scale. So, it is very important that extensive sampling soil moisture of the surface heterogeneous and effective upscaling multi-point in situ soil moisture to remote sensing pixel scale. However, it is very difficult to collect them extensively if the soil moisture signal is complicated or dynamically changing. Considering the sparsity of soil moisture and the effects of observation noise, this paper models the linear programming problem between the soil moisture remote sensing pixel and in-situ sampling data using hierarchical non-parametric Bayesian linear regression. This model does not assume that the specific distribution of regression parameters which will be learned adaptively by the nonparametric Bayesian method. In addition, we implement the Dirichlet process to exploit the spatial similarity of the in-situ sampling data of soil moisture, thus to improve the spatial upscaling accuracy. Due to the Dirichlet process without explicit mathematical expression, the model of the posteriori probability distribution is very hard to deal with. To this end, the Gibbs sampling scheme based on MCMC (Markov Chain Monte Carlo) is adopted to infer the optimal regression weighting coefficient, and the spatial scale of the soil moisture in situ sampling is effectively upscaled. The experimental results show that the spatial upscaling method of non-parametric Bayesian linear regression is closer to the observed remote sensing pixel scale and better than the state of the art Bayesian method and Kriging method.
机译:在土壤水分遥感产品地面验证中,土壤水分原位采样是异类的,并且与遥感像素尺度不一致。因此,对表面异质性土壤水分进行大量采样并有效地将多点原位土壤水分放大至遥感像素规模非常重要。但是,如果土壤水分信号复杂或动态变化,则很难大量收集它们。考虑到土壤水分的稀疏性和观测噪声的影响,本文采用分层非参数贝叶斯线性回归模型对土壤水分遥感像素与原位采样数据之间的线性规划问题进行了建模。该模型不假定将通过非参数贝叶斯方法自适应地学习回归参数的特定分布。此外,我们利用Dirichlet过程来利用土壤水分原位采样数据的空间相似性,从而提高空间放大精度。由于Dirichlet过程没有明确的数学表达式,因此后验概率分布模型很难处理。为此,采用基于MCMC(马尔可夫链蒙特卡洛)的吉布斯采样方案来推导最佳回归加权系数,并有效地提高了土壤水分原位采样的空间尺度。实验结果表明,非参数贝叶斯线性回归的空间放大方法更接近于观测到的遥感像素尺度,并且优于现有的贝叶斯方法和克里格方法。

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