Multi-frequency polarimetric microwave observations of snow cover on first-year Arctic sea ice

V. Nandan, John J. Jacket, J. P. Gill, T. Geldsetzer, M. Fuller
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引用次数: 0

Abstract

This study explores the potential of a multi-frequency (Ku-, X- and C-band) scatterometry approach, to understand microwave interactions between teo statistically different snow thickness covers (14cm and 8cm) on first-year Arctic sea ice during the late winter to early-melt season transition. The results show substantial differences in backscatter response from all three frequencies, for both snow covers. Highly-saline snow covers with fluctuating snow geophysical and thermodynamic properties cause these backscatter fluctuations, with contributions from surface and volume scattering from different snow layers and interfaces. C-band exhibited drastic variations in backscatter, especially for the 14cm snow cover, when compared to Ku- and X-band. In the case of 8cm snow cover, all the three frequencies show minimal sensitivity to snow electro-thermo-physical properties. Our results show distinctly different snow thermodynamic processes operating within the different snow layers, essential for snow thickness estimation on first-year sea ice using active microwave remote sensing approaches.
北极海冰第一年积雪覆盖的多频极化微波观测
本研究探索了多频率(Ku, X和c波段)散射测量方法的潜力,以了解在冬末到融冰季早期过渡期间,统计上不同积雪厚度(14厘米和8厘米)在北极海冰上第一年的微波相互作用。结果表明,两种积雪在所有三种频率下的后向散射响应存在显著差异。具有波动雪的地球物理和热力学性质的高盐积雪覆盖引起了这些后向散射波动,不同雪层和界面的表面和体积散射对这些波动有贡献。与Ku波段和x波段相比,c波段的后向散射变化较大,特别是在14cm积雪范围内。在8厘米积雪的情况下,所有三个频率对雪的电-热-物理特性都表现出最小的敏感性。我们的研究结果表明,不同雪层内运行的雪热力过程存在明显差异,这对于利用主动微波遥感方法估算第一年海冰的雪厚至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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