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UW-Scat: A Ground-Based Dual-Frequency Scatterometer for Observation of Snow Properties

机译:UW-Scat:基于地面的双频散射仪,用于观测积雪

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摘要

The University of Waterloo scatterometer, which is a system developed for observation of snow and ice properties, is described. The system is composed of two frequency-modulated continuous-wave radars operating at center frequencies of 17.2 and 9.6 GHz. A field-deployable platform allows a rapid setup and observation at remote sites under harsh environmental conditions. A two-axis positioning system moves the radar beam across a user-programmable range of azimuth ($pm 180^{circ}$) and elevation angles (15$^{circ}$–105 $^{circ}$). Typical azimuth scans of 60 $^{circ}$ angular width generate between 21 and 586 independent samples, depending on the wavelength and the elevation angle. The backscatter response of terrestrial snow in the Canadian Subarctic is demonstrated with two experiments conducted in Churchill, MB, Canada, between 2009 and 2011.
机译:描述了滑铁卢大学散射仪,该散射仪是为观察冰雪性质而开发的系统。该系统由两个工作在中心频率为17.2和9.6 GHz的调频连续波雷达组成。可现场部署的平台允许在恶劣的环境条件下在偏远地区进行快速设置和观察。两轴定位系统可在用户可编程的方位角($ pm 180 ^ {circ} $)和仰角(15 $ ^ {circ} $ – 105 $ ^ {circ} $)范围内移动雷达波束。取决于波长和仰角,典型的60度角宽度的方位角扫描会生成21到586个独立样本。 2009年至2011年之间,加拿大MB丘吉尔市进行了两次实验,证明了加拿大亚北极地区陆雪的反向散射响应。

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