Research on Influence of Charged Sand Atmosphere on the Performance of Ku and Ka Band Radar

Yang Ruike, Yue Xilin, Wu Fuping, Liu Renxian, Z. Ye
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Abstract

In arid and semi-arid areas, in the atmosphere carrying sand particles, in order to make the radar work all-weather, it is necessary to research the properties of microwave propagation in the sand atmosphere and the impact on the radar performance. The absorption, scattering and backscattering of sand particles carrying different size and different charge are analyzed by Mie theory. At K and Ka band, using the log-normal particle size distribution spectrum in sand atmosphere with different visibility, the specific attenuation and the backscattering per unit volume of charged sand particle are studied. Based on meteorological radar equation, the radar echo power and radar reflectivity are analyzed, and the relations between they with visibility and particle charge are given. The results show that the charged particle in the sand atmosphere increases the microwave attenuation. The attenuation reaches a maximum when the charge-to-mass ratio is about 50uC/kg. When the amount of sand particle charge increases, the backscattering factor increases. The radar echo power of the sand atmosphere increases with the decrease of visibility, but when the distance is greater than a certain distance, due to the increase of attenuation, it decreases with the visibility decrease. The effect of charged particle in sand atmosphere becomes larger with increasing frequency and distance. This study can lay a good foundation for radar detection in sand and dust atmosphere, and inversion of the physical properties of the sand atmosphere.
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带电沙大气对Ku和Ka波段雷达性能影响的研究
在干旱半干旱地区,大气中携带沙粒,为了使雷达全天候工作,有必要研究微波在沙质大气中的传播特性及其对雷达性能的影响。用Mie理论分析了不同粒径、不同电荷的砂粒的吸收、散射和后向散射。在K和Ka波段,利用不同能见度的沙尘大气中的对数正态粒径分布谱,研究了带电沙尘的比衰减和单位体积的后向散射。根据气象雷达方程,分析了雷达回波功率和雷达反射率,并给出了它们与能见度和粒子电荷的关系。结果表明,沙质大气中的带电粒子增加了微波衰减。当电荷质量比约为50uC/kg时,衰减达到最大。随着砂粒电荷量的增加,后向散射系数增大。沙尘大气雷达回波功率随能见度降低而增大,但当距离大于一定距离时,由于衰减增大,随能见度降低而减小。沙尘大气中带电粒子的作用随频率和距离的增加而增大。该研究可为沙尘大气雷达探测及沙尘大气物理性质的反演奠定良好的基础。
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