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首页> 外文期刊>Antennas and Propagation, IEEE Transactions on >Measurements of In-Flight Cross-Track Antenna Patterns of Radar Depth Sounder/Imager
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Measurements of In-Flight Cross-Track Antenna Patterns of Radar Depth Sounder/Imager

机译:雷达深度测深仪/成像仪的飞行中跨轨天线方向图的测量

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摘要

Antenna arrays with low sidelobes in the cross-track direction are needed for sounding and imaging ice-sheets margins including outlet glaciers. Weak radar signals from the ice-bed interface are often masked by off-vertical surface clutter from extremely rough crevassed surfaces in ice-sheet margins. Synthetic aperture radar (SAR) processing can be used to synthesize a large array for reducing clutter in the along-track direction. Low-sidelobe transmit- and receive-antenna patterns must be generated from a limited size array in the cross-track direction. Airborne antenna pattern measurements are critical to verifying pattern characteristics in the presence of a non-ideal ground plane and neighboring aircraft structures, as well as in-flight operational dynamics. In this paper, we describe a set of airborne measurements performed to determine and optimize antenna patterns for the very high frequency (VHF) array used to sound and image polar ice sheets. We measured antenna patterns by flying over a relatively smooth ice surface at an altitude of about 2700 m. The pattern data were obtained by processing the surface echoes with aircraft rolled from left to right over more than five cycles. We also simulated antenna patterns using a three-dimensional computer model of the entire airborne platform and compared with experimental results. The discrepancies between the measured and simulated results are less than 2.7 dB for 85% of the data samples. The measured pattern data will be used to optimize our array processing algorithms.
机译:在跨轨方向上具有低旁瓣的天线阵列对于探测和成像包括出口冰川的冰盖边缘是必需的。来自冰床界面的弱雷达信号通常被来自冰盖边缘极其粗糙的皱纹表面的非垂直表面杂波所掩盖。合成孔径雷达(SAR)处理可用于合成大型阵列,以减少沿航迹方向的混乱情况。低旁瓣发射和接收天线方向图必须从交叉轨道方向上的有限大小阵列中生成。机载天线方向图测量对于在不理想的地面和相邻飞机结构的情况下验证方向图特性以及飞行中的运行动力学至关重要。在本文中,我们描述了一组空中测量,旨在确定和优化用于对极地冰盖进行声音和成像的甚高频(VHF)阵列的天线方向图。我们通过在大约2700 m的相对光滑的冰面上飞行来测量天线方向图。图案数据是通过处理飞机从左向右滚动超过五个周期的表面回波获得的。我们还使用整个机载平台的三维计算机模型模拟了天线方向图,并与实验结果进行了比较。对于85%的数据样本,测量结果与模拟结果之间的差异小于2.7 dB。测得的图案数据将用于优化我们的阵列处理算法。

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