崔生成, 朱文越, 杨世植, 李学彬. 基于正则化的地表反射特性参数反演方法[J]. 武汉大学学报 ( 信息科学版), 2018, 43(8): 1264-1270. DOI: 10.13203/j.whugis20160244
引用本文: 崔生成, 朱文越, 杨世植, 李学彬. 基于正则化的地表反射特性参数反演方法[J]. 武汉大学学报 ( 信息科学版), 2018, 43(8): 1264-1270. DOI: 10.13203/j.whugis20160244
CUI Shengcheng, ZHU Wenyue, YANG Shizhi, LI Xuebin. Regularization-Based Retrieval Method for Surface Reflective Property Parameters[J]. Geomatics and Information Science of Wuhan University, 2018, 43(8): 1264-1270. DOI: 10.13203/j.whugis20160244
Citation: CUI Shengcheng, ZHU Wenyue, YANG Shizhi, LI Xuebin. Regularization-Based Retrieval Method for Surface Reflective Property Parameters[J]. Geomatics and Information Science of Wuhan University, 2018, 43(8): 1264-1270. DOI: 10.13203/j.whugis20160244

基于正则化的地表反射特性参数反演方法

Regularization-Based Retrieval Method for Surface Reflective Property Parameters

  • 摘要: 区域和全球尺度下研究气候变化,需要准确描述大气边界层处下垫面地表的光反射特性。为此,提出基于正则化的约束反演方法,其核心在于正则化参数的选取。通过L曲线拐点位置的确定,求出最合适的正则化约束参数,以稳定陆表反射特性参数的定量反演。京津唐地区数值反演试验与熵减分析结果表明,可见光红通道和近红外通道的信息指数分别为11.682 2和10.072 6;基于L曲线的地物反射特性正则化反演前后,两个通道的平均信息指数增量分别为0.440 0和0.354 6,最大增量为2.467 2和2.290 5。L曲线正则化方法的优势在于其不依赖于地表参数的先验知识,可有效解决卫星观测信息不足时地表参数的反演问题。

     

    Abstract: Climate studies at regional and global scales, require accurate descriptions of the light reflecting behaviors of the underlying surfaces at atmospheric boundary layers. A regularized constraint retrieval method is correspondingly proposed for this purpose. The key to the presented method is the determination of the regularization parameter (RP). In order to stabilize the quantitative retrievals of land surface reflective property (SRP) parameters, the optimized RP is obtained via the corner point of the L-curve. Numerical retrieval tests in Beijing-Tianjin-Tangshan region and entropy reduction results suggest that information indices in visible-red and near-infrared channels reach 11.682 2 and 10.072 6; and that the average information indices in these two channels, before and after SRP retrie-vals using L-curve-based regularization (RLC) method, are 0.440 0 and 0.354 6, with the greatest increase reaching 2.467 2 and 2.290 5, respectively. The advantage of the RLC method lies in the independence of the a priori surface parameters knowledge. The RLC method is very effective and useful for the retrievals of surface parameters in the cases of insufficient satellite observations.

     

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