Phase shift of the electromagnetic waves due to dry snow

C. Ventrice, S. C. Fares, M. A. Fares
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Abstract

Based on the point matching technique, the phase shift of the electromagnetic waves due to dry snow is computed. The analysis is restricted to the forward-scattering direction from oblate spheroidal dry snow. Numerical results are obtained for two orthogonal polarizations of the incident wave. The calculations are made for various microwave frequencies, between 6 and 100 GHz, and also for different precipitation rates, between 0.5 and 3 mm/hr. The effect of the frequency and the precipitation rate on the phase shift is examined. It is found that at a fixed value of the precipitation rate, the phase shift of both polarizations decreases with increasing frequency. It is also observed that at a fixed frequency, the phase shift of both polarizations decreases with increasing precipitation rate. The differential phase shift is found to follow the same trend as the phase shift for frequencies greater than 20 GHz and are negligible for frequencies below 20 GHz. In addition, it is found that the phase shift of snow decreases with snow wetness for fixed precipitation rate and frequency.
由于干雪引起的电磁波相移
基于点匹配技术,计算了干雪作用下电磁波的相移。分析仅限于扁球状干雪的前向散射方向。得到了入射波的两个正交偏振的数值结果。这些计算是在不同的微波频率下进行的,在6到100 GHz之间,也在不同的降水速率下进行的,在0.5到3毫米/小时之间。研究了频率和析出速率对相移的影响。结果表明,在一定的析出速率下,两种极化相移随频率的增加而减小。在固定频率下,两种极化相移均随析出速率的增加而减小。发现微分相移与大于20ghz频率的相移遵循相同的趋势,并且对于低于20ghz的频率可以忽略不计。此外,在固定降水率和频率下,雪的相移随雪湿度的增加而减小。
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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