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首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Springtime C-band SAR backscatter signatures of Labrador Sea marginal ice: measurements versus modeling predictions
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Springtime C-band SAR backscatter signatures of Labrador Sea marginal ice: measurements versus modeling predictions

机译:拉布拉多海边缘冰的春季C波段SAR背向散射特征:测量与建模预测

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During the March 1987 Labrador Ice Margin Experiment (LIMEX '87) two independent investigations were conducted to determine the C-band backscattering cross section of the marginal pack ice along the Newfoundland coast. In one experiment, data from a recently calibrated C-band airborne scatterometer were combined with C-band synthetic aperture radar (SAR) data to measure the normalized scattering cross section of the ice at incidence angles from 10 degrees to 74 degrees to within +or-2 dB. In the other experiment, detailed measurements of ice surface roughness and surface properties were made and the radar cross sections were predicted from a scattering model. In the present study, measured and model results are combined and shown to be fully compatible. By extension, the results are expected to apply to any rubbled sea-ice surface when surface scattering dominates.
机译:在1987年3月的拉布拉多冰缘实验(LIMEX '87)期间,进行了两次独立调查,以确定纽芬兰海岸沿边缘冰块的C波段反向散射截面。在一个实验中,将来自最近校准的C波段机载散射仪的数据与C波段合成孔径雷达(SAR)数据结合起来,以测量入射角从10度到74度到+或以内的冰的归一化散射截面。 -2 dB。在另一个实验中,对冰的表面粗糙度和表面特性进行了详细的测量,并根据散射模型预测了雷达的横截面。在本研究中,将测量结果和模型结果结合起来并显示出完全兼容。通过扩展,当表面散射占主导地位时,预期结果将适用于任何碎石海冰表面。

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