Measurements of Radio Star and Satellite Scintillations at a Subauroral Latitude

R. Allen, J. Aarons, H. Whitney
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引用次数: 3

Abstract

Observations of two radio stars, Cygnus A and Cassiopeia A, and of two satellites, Cosmos I and Transit 4A, have yielded data on lower and upper atmospheric irregularities. The frequencies studied have included 20 Mc, 40 Mc and 54 Mc for satellite transmissions, and 30 Mc to 3000 Mc for radio star signals. The antennas used have ranged from a dipole to a 150-foot parabola. The irregularities in refractive index in the lower atmosphere produce amplitude fluctuations up to several times average with a fading rate of 3 to 0.5 per minute while ionospheric amplitude fluctuations can increase several decibels, with rates from 1 to 60 per minute. Lower atmosphere scintillation rates increase as the elevation angle increases and generally disappear above 50 of elevation. During intense magnetic storms, the ionospheric scintillation rate is a function of wavelength in the UHF range. Ionospheric scintillations are functions of both magnetic conditions and of the subionospheric latitudes of the irregularities; they are observed at zenith at the geomagnetic latitude of the Sagamore Hill Radio Observatory (54°). Using spaced receivers, heights of single irregularities have ranged from about 100 to 600 km and representative sizes from about 0.1 to 4 km. Irregularities constitute the prime factor affecting the level, phase and angle of arrival of signals propagated through the auroral regions.
在亚极光纬度测量无线电星和卫星闪烁
对两颗射电恒星——天鹅座A和仙后座A,以及两颗卫星——宇宙一号和凌日四号4A的观测,已经获得了低层和高层大气不规则性的数据。所研究的频率包括卫星传输的20、40和54兆赫,以及射电星信号的30至3000兆赫。所使用的天线从偶极到150英尺的抛物线不等。低层大气中折射率的不规则性产生的振幅波动可达平均值的数倍,衰减速率为每分钟3至0.5,而电离层的振幅波动可增加数分贝,衰减速率为每分钟1至60分贝。低层大气闪烁率随仰角增加而增加,一般在仰角50以上消失。在强磁暴期间,电离层闪烁率是波长在UHF范围内的函数。电离层闪烁是磁场条件和不规则的亚电离层纬度的函数;它们是在Sagamore Hill射电天文台地磁纬度(54°)的天顶观测到的。使用间隔接收器,单个不规则的高度约为100至600公里,代表性大小约为0.1至4公里。不规则性是影响通过极光区域传播的信号的水平、相位和到达角度的主要因素。
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