雪崩样雪运动的FMCW雷达成像

M. Ash, K. Chetty, P. Brennan, J. McElwaine, C. Keylock
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引用次数: 26

摘要

为了校准计算模型,需要高质量的雪崩流现场测量,而计算模型是管理雪崩流所构成威胁的重要工具。本文介绍了一种由伦敦大学学院研制的用于采集高分辨率雪崩流数据的新型c波段FMCW雷达系统。该雷达采用全脱模硬件架构、多种频率坡道和8通道接收器阵列。我们还展示了使用部署在雪滑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。结果以距离-时间图的形式呈现。对重力作用下的预期流速进行了简单计算,结果与实验估计值吻合。结果表明,该雷达系统能够记录雪运动的高距离分辨率微波图像。这里报告的实验是作为雷达系统全面试验的先驱进行的,在此期间,将捕获全尺寸雪崩流的图像。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
FMCW radar imaging of avalanche-like snow movements
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 highresolution 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.
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