首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Observation of sea-ice thickness in the sea of Okhotsk by using dual-frequency and fully polarimetric airborne SAR (pi-SAR) data
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Observation of sea-ice thickness in the sea of Okhotsk by using dual-frequency and fully polarimetric airborne SAR (pi-SAR) data

机译:利用双频和全极化机载SAR(pi-SAR)数据观测鄂霍次克海的海冰厚度

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摘要

To investigate the possibilities of using dual-frequency, multipolarization synthetic aperture radar (SAR) data to monitor sea ice, we derived the relationship between various polarization characteristics and the physical parameters of sea ice. We discuss the frequency and polarization characteristics of the backscattering coefficients of sea ice and then characterize its thickness by comparing the corresponding backscattering coefficient for each polarization with the physical parameters of the ice. We first propose a methodology for classifying sea-ice types by using a polarimetric decomposition technique, before comparing an estimation of the sea-ice thickness with the corresponding dual-frequency, multipolarization SAR data. We utilized the backscattering ratio to estimate the thickness of the sea ice. This ratio canceled the effect of roughness on the backscattering. The method was validated using Pi-SAR (polarimetric and interferometric airborne SAR) observation data obtained at ground-truth sites.
机译:为了研究使用双频,多极化合成孔径雷达(SAR)数据监测海冰的可能性,我们推导了各种极化特征与海冰物理参数之间的关系。我们讨论了海冰后向散射系数的频率和极化特性,然后通过将每种极化的相应后向散射系数与冰的物理参数进行比较来表征海冰的厚度。在将海冰厚度的估计值与相应的双频,多极化SAR数据进行比较之前,我们首先提出一种使用极化分解技术对海冰类型进行分类的方法。我们利用反向散射比估算海冰的厚度。该比率消除了粗糙度对反向散射的影响。该方法已通过在真实地面获得的Pi-SAR(极化和干涉空中SAR)观测数据进行了验证。

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