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Passive microwave signatures of autumnal sea ice types from ship-based observation

机译:船舶观察中秋季海冰类型的被动微波特征

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Surface-scale passive microwave signatures of newly formed sea ice were collected using ship-based radiometers in the Southern Beaufort Sea and Amundsen Gulf between mid October and mid November 2003. Sea ice in the region was highly spatially and temporally variable. Over a heterogeneous area of open water and thin ice, polarization ratios showed multimodal frequency distributions and the differences between surface and satellite radiometric data were large. However, differences were small over a homogeneous area of snow-covered first-year ice during late fall and the corresponding histograms showed unimodal distributions. Our results suggest that subpixel heterogeneity is a critical factor in characterizing the mixture rules used in passive microwave sea ice algorithms.
机译:在2003年11月中旬和2003年11月中旬之间使用船舶辐射米和Amundsen海湾的船舶辐射仪收集了新成立的海冰的表面鳞片被动微波签名。该地区的海冰在空间上高度空间和时间变化。在开放水和薄冰的异质区域上,偏振比显示多峰频率分布,表面和卫星辐射数据之间的差异很大。然而,在晚秋季的冰川覆盖的第一年冰上的均匀区域差异很小,相应的直方图显示了单峰的分布。我们的研究结果表明,子像素异质性是表征被动微波海冰算法中使用的混合规则的关键因素。

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