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Calibrating an imaging riometer: determination of the true beam azimuth angle position

机译:校准成像测力仪:确定真实的光束方位角位置

摘要

An imaging riometer uses the absorption of cosmic radio noise as a means of measuring electron density enhancements in the D region of the ionosphere. It employs a ground-based phased antenna array to produce narrow beams which typically observe a region 200 by 200 km at 90 km altitude. Imaging riometers have traditionally been used for studying energetic electron precipitation into the D region and have also recently been used to characterize mesospheric gravity waves. Determining the location and shape of the riometer beam pattern projected onto the ionosphere is therefore important because it allows the spatial distribution of space weather effects to be accurately visualized and also because it would allow mesospheric gravity wave characteristics to be accurately quantified. Currently, the beam patterns of imaging riometers are determined theoretically, and attempts have been made to validate them by comparison with cosmic radio maps of low spatial resolution; alternatively, they are determined by calibration overflights using aircraft in a complex and expensive procedure. Here we demonstrate a novel wavelet-based approach to accurately determine the azimuth angle of each imaging riometer beam from the riometer data itself using quiet day observations alone and by way of example show how the actual beam azimuth angles (pointing directions) of the Halley (76°S, 27°W) 49-beam imaging riometer vary from those expected using theoretical calculations.
机译:成像测距仪将吸收宇宙无线电噪声作为测量电离层D区域电子密度增强的一种手段。它采用基于地面的相控天线阵列来产生窄波束,通常在90 km的高度观察200×200 km的区域。传统上,成像测距仪用于研究高能电子向D区域的沉淀,最近还用于表征中层重力波。因此,确定投影到电离层上的变径辐射束方向图的位置和形状很重要,因为它可以精确显示空间天气效应的空间分布,并且还可以精确量化中层重力波的特征。目前,成像测距仪的光束方向图是从理论上确定的,并且已经尝试通过与低空间分辨率的宇宙无线电图进行比较来验证它们。或者,它们是通过使用飞机以复杂且昂贵的程序进行校准飞越来确定的。在这里,我们展示了一种新颖的基于小波的方法,该方法可以仅使用安静的一天观测来从测速仪数据本身准确地确定每个成像测速仪光束的方位角,并通过示例的方式展示哈雷的实际光束方位角(指向方向)( 76束,27°W)的49束成像测距仪与使用理论计算得出的结果有所不同。

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