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电波极化面旋转特性研究
引用本文:赵红梅,江长荫,王健.电波极化面旋转特性研究[J].空间科学学报,2011,31(2):208-213.
作者姓名:赵红梅  江长荫  王健
作者单位:1.中国电波传播研究所, 青岛266107
基金项目:国家科技重大专项基金项目资助
摘    要:推导了电波极化面旋转角表达式, 利用实测电子浓度、地磁场磁感应强度模与磁倾角剖面,对定高载体、不同天线侧视方向与地球法线夹角、不同地区、不同频段、不同时段、不同太阳活动情况下的电波极化面旋转角进行了仿真, 并对仿真结果进行了分析, 得出了电波极化面旋转角的时域、地域、频域等规律和特性. 为这一领域的深入研究提供了参考. 

关 键 词:电离层    双折射    电波极化面旋转
收稿时间:1900-01-01

Analysis of Properties for Radiowave Polarization Plane Rotation
ZHAO Hongmei,JIANG Changyin,WANG Jian.Analysis of Properties for Radiowave Polarization Plane Rotation[J].Chinese Journal of Space Science,2011,31(2):208-213.
Authors:ZHAO Hongmei  JIANG Changyin  WANG Jian
Institution:1.China Research Institute of Radiowave Propagation, Qingdao 2661072.China Research Institute of Radiowave Propagation, Xinxiang 453003
Abstract:The radiowave polarization plane rotation is caused by the ionospheric dispersion and the double refraction. Begin with the ionosphere refraction index, the formula of radiaowave polarization plane rotation angle is derived in this paper. Using the measured electron density, magnetic induction intensity module of geomagnetic field, and magnetic obliquity profiles, the radiaowave polarization plane rotation angle is simulated for fixed height carrier under different angles between antenna side-view and earth normal, different regions, different frequency bands, different time slots, and different solar activity cases, which is described by column diagraphs and tables. The simulation results and the rules and properties of radiowave polarization plane rotation angle are analyzed and summarized in its seasonal, temporal, regional, frequency-domain aspects. (1) The rotation angle will decrease as the frequency arises, and will increase as the angle between antenna side-view and earth normal arises. (2) The rotation angle will increase as the sun polar activity arises, larger in the day and smaller at night. (3) At night, the rotation angle in summer is the largest and in winter is the smallest as in high and middle latitude, larger in spring and autumn and smaller in summer and winter as in low latitude. (4) In the day, the rotation angle in winter and spring is larger that in summer and autumn as in high latitude, larger in spring and autumn and smaller in summer and autumn. 
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