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A low power consumption radar system for measuring ice thickness and snow/firn accumulation in Antarctica

机译:一种低功耗雷达系统,用于测量南极洲的冰厚度和积雪/积雪

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摘要

In order to measure total ice thickness and surface snow accumulation in Antarctica, wehave designed and built a surveying system comprising two types of radar. This system is aimed at havinglow power consumption, low weight/volume and low construction cost. The system has a pulsecompressionradar to measure ice thickness, and a frequency-modulated continuous wave (FM-CW)radar designed to measure hundreds of meters of surface snow/firn layers with high resolution. The pulsecompressionradar operates at 155 MHz, 20MHz of bandwidth; and the FM-CW radar operates from 550to 900 MHz. The system was tested in December 2010 at Union Glacier (798460 S, 838240 W), WestAntarctica, during an oversnow campaign, where Union and other nearby glaciers (Schanz, Schneiderand Balish) were covered through 82km of track. Ice thickness of 1540m and snow/firn thickness of120m were detected in the area. The collected data allowed the subglacial topography, internal icestructure, isochronous and the snow/ice boundary layer to be detected. Here we describe radarelectronics, their main features and some of the results obtained during the first test campaign. Furtherimprovements will focus on the adaptation of the system to be implemented on board airplane platforms.
机译:为了测量南极洲的总冰厚和地表积雪,我们设计并构建了一种包括两种雷达的测量系统。该系统旨在具有低功耗,低重量/体积和低建造成本。该系统具有测量冰厚的脉冲压缩雷达和设计用于测量高分辨率的数百米地表雪/碎屑层的调频连续波(FM-CW)雷达。脉冲压缩雷达的工作频率为155 MHz,带宽为20MHz。 FM-CW雷达的工作频率为550至900 MHz。该系统于2010年12月在一场超雪运动中在西极洲的联合冰川(798460 S,838240 W)上进行了测试,该联合会及其他附近的冰川(Schanz,Schneiderand Balish)被82公里的轨道覆盖。在该地区检测到冰厚为1540m,雪/雪厚度为120m。收集的数据可以检测到冰下地形,内部冰结构,等时线和雪/冰边界层。在这里,我们描述了雷达电子设备,其主要功能以及在首次测试活动中获得的一些结果。进一步的改进将集中在将要在飞机平台上实施的系统的适应性上。

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