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Decomposition of SMAP polarization ratio into surface soil moisture and vegetation dynamics

机译:将SMAP极化比分解为地表土壤水分和植被动力学

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In this study we examined the linear decomposition and relationship between the SMAP observed Polarization Ratio into surface soil moisture and vegetation. Temporal linear regression, per each SMAP pixel, is performed to estimate the decomposition coefficients. Variances (explained variance) in PR is predominantly dominated by dynamics of surface soil moisture and degrades with increasing vegetation amount. Although PR, by itself, is high in arid and semi-arid regions, due to lack of moisture and vegetation dynamics, the explained variance is very small.
机译:在这项研究中,我们研究了线性分解以及SMAP观测到的极化比与表层土壤水分和植被之间的关系。对每个SMAP像素执行时间线性回归以估计分解系数。 PR的方差(解释方差)主要由表层土壤水分的动力学决定,并随着植被数量的增加而降低。尽管PR本身在干旱和半干旱地区较高,但由于缺乏水分和植被动态,所解释的方差很小。

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