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Polarization anomaly of the microwave brightness temperature from ice

机译:冰微波亮度温度的极化异常

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Brightness temperatures over sea ice and water surfaces derived from vertically polarized microwave signals are normally higher than the values resulting from horizontally polarized signals. But, according to simple model considerations, this normal relationship can be reversed for three adjacent layers (atmosphere, ice, and water) with different dielectric properties. The validity of this concept is confirmed by measurements near the ice surface. It is found that the polarization anomaly results from the interference of the polarized microwaves from different interfaces. (C) 1998 Optical Society of America. [References: 4]
机译:通常,由垂直极化的微波信号得出的海冰和水面上的亮度温度通常高于由水平极化的信号得出的温度。但是,根据简单的模型考虑,对于具有不同介电特性的三个相邻层(大气层,冰层和水层),可以颠倒这种正常关系。这一概念的有效性通过在冰面附近的测量得到证实。发现极化异常是由于极化微波受到不同界面的干扰引起的。 (C)1998年美国眼镜学会。 [参考:4]

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