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FMCW radar imaging of avalanche-like snow movements

机译:FMCW雷达成像像雪崩般的雪运动

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High quality field measurements of avalanche flows are required for calibrating computational models which are an essential tool in managing the threat posed by these flows. In this paper we present a new C-band FMCW radar system developed at University College London for gathering high-resolution avalanche flow data. The radar employs a full deramp hardware architecture, a diverse set of frequency ramps, and an 8-channel receiver array. We also show initial results of a small-scale field trial carried out using a single channel prototype radar deployed in a snow chute. The results are presented as range-time plots. A simple calculation of the expected flow velocity due to gravity agrees with the estimated experimental value. The results demonstrate the capability of the radar system to record high range resolution microwave images of snow movements. The experiments reported here were carried out as a precursor to full trials of the radar system during which images of full scale avalanche flows will be captured.
机译:为了校准计算模型,雪崩流需要进行高质量的现场测量,这是管理这些流带来的威胁的必不可少的工具。在本文中,我们介绍了伦敦大学学院开发的一种新的C波段FMCW雷达系统,用于收集高分辨率雪崩流数据。雷达采用完整的deramp硬件架构,各种频率斜坡和8通道接收器阵列。我们还显示了使用部署在雪道中的单通道原型雷达进行的小规模现场试验的初步结果。结果以范围-时间图表示。重力引起的预期流速的简单计算与估算的实验值一致。结果表明,雷达系统具有记录雪运动的高分辨率微波图像的能力。此处报告的实验是对雷达系统进行全面试验的先驱,在此期间将捕获全尺寸雪崩流的图像。

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