波弗特海海冰的偏振遥感研究

S. Nghiem, R. Kwok, M. Drinkwater
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引用次数: 1

摘要

数据在1988年3月用喷气推进实验室(JPL)偏振机载合成孔径雷达(SAR)收集。在充分考虑极化定标的情况下,从散射数据中得到了完整的协方差矩阵。这些图像经过处理后形成了波弗特海的海冰场景。这些场景包含各种冰类型,包括薄冰、厚一年冰和多年冰。将海冰建模为一层随机介质,利用强涨落理论得到的有效介电常数,在畸变玻恩近似下计算海冰极化后向散射系数。通过比较不同入射角下的海冰特征与理论模型的结果,对JPL SAR在Beaufort海冰场景上远程观测到的海冰特征进行了解释。
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Polarimetric Remote Sensing of Sea Ice in the Beaufort Sea
Data were collected in March 1988 with the Jet Propulsion Laboratory (JPL) polarimetric airborne synthetic aperture radar (SAR). Full covariance matrices were obtained from the scattering data with proper consideration of the polarimetric calibration. Images were processed to form the sea ice scenes in the Beaufort sea. These scenes contain various ice types including thin ice, thick first-year ice, and multiyear ice. Sea ice was modeled as a layer random medium and the polarimetric backscattering coefficients were calculated under the distorted Born approximation with effective permittivities obtained from the strong fluctuation theory. Sea ice signatures remotely observed by the JPL SAR over the Beaufort sea ice scenes were interpreted by comparing their behavior at different incident angles with results obtained from the theoretical model.
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