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Scattering phenomenology of arctic lake ice

机译:北极湖冰的散射现象学

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摘要

This paper presents the radar scattering phenomenology of arctic shallow lake ice. This is an important feature for monitoring the arctic climate for this purpose, a full-wave simulation model to analyze lake ice scattering that includes columnar air bubbles and rough interface is presented. The proposed model can handle complex interactions between high density air bubbles and rough ice surfaces. Based on this model, the scattering contributions from the rough ice/water interface and columnar air bubbles in the ice at C band are calculated. It is concluded that the roughness at the interface between ice and water is the dominate contributor to the observed backscatter.
机译:本文介绍了北极浅湖冰的雷达散射现象学。这是为此目的监测北极气候的重要特征,一种全波仿真模型,用于分析湖冰散射,包括柱状气泡和粗糙接口。所提出的模型可以处理高密度气泡和粗糙冰表面之间的复杂相互作用。基于该模型,计算C频段冰冰/水界面和冰柱气泡的散射贡献。结论是,冰与水之间的界面的粗糙度是对观察到的反向散射的贡献者。

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