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Upward-looking L-band FMCW radar for snow cover monitoring

机译:向上看的L波段FMCW雷达用于积雪监测

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摘要

Forecasting snow avalanche danger in mountainous regions is of major importance for the protection of infrastructure in avalanche run-out zones. Inexpensive measurement devices capable of measuring snow height and layer properties in avalanche starting zones may help to improve the quality of risk assessment. We present a low-cost L-band frequency modulated continuous wave radar system (FMCW) in upward-looking configuration. To monitor the snowpack evolution, the radar system was deployed in fall and subsequently was covered by snowfalls. During two winter seasons we recorded reflections from the overlying snowpack. The influence of reflection magnitude and phase to the measured frequency spectra, as well as the influence of signal processing were investigated. We present a method to extract the phase of the reflection coefficients from the phase response of the frequency spectra and their integration into the presentation of the measurement data. The phase information significantly improved the detectability of the temporal evolution of the snow surface reflection. We developed an automated and a semi-automated snow surface tracking algorithm. Results were compared with independently measured snow height from a laser snow-depth sensor and results derived from an upward-looking impulse radar system (upGPR). The semi-automated tracking used the phase information and had an accuracy of about 6 to 8 cm for dry-snow conditions, similar to the accuracy of the upGPR, compared to measurements from the laser snow-depth sensor. The percolation of water was observable in the radargrams. Results suggest that the upward-looking FMCW system may be a valuable alternative to conventional snow-depth sensors for locations, where fixed installations above ground are not feasible.
机译:预测山区雪崩的危险对于雪崩流失地区的基础设施保护至关重要。能够测量雪崩起始区的雪高和层特性的廉价测量设备可能有助于提高风险评估的质量。我们提出了一种外观向上的低成本L波段频率调制连续波雷达系统(FMCW)。为了监视积雪的演变,该雷达系统于秋季部署,随后被降雪覆盖。在两个冬季,我们记录了上覆雪堆的反射。研究了反射幅度和相位对所测频谱的影响以及信号处理的影响。我们提出了一种从频谱的相位响应中提取反射系数相位并将其积分到测量数据表示中的方法。相位信息显着提高了雪面反射时间演变的可检测性。我们开发了一种自动和半自动雪面跟踪算法。将结果与激光雪深传感器独立测量的雪高进行比较,并将结果从向上看的脉冲雷达系统(upGPR)获得。与来自激光雪深传感器的测量结果相比,半自动跟踪使用了相位信息,在干雪条件下的精度约为6至8厘米,类似于upGPR的精度。在雷达图中可以观察到水的渗透。结果表明,对于无法在地面上固定安装的位置,具有前瞻性的FMCW系统可能是传统雪深传感器的有价值的替代品。

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