High density coverage investigation of The Austre LovénBreen (Svalbard) using Ground Penetrating Radar

A. Saintenoy, J. Friedt, F. Tolle, E. Bernard, D. Laffly, C. Marlin, M. Griselin
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引用次数: 5

Abstract

A three week field survey over April 2010 allowed for the acquisition of 120 Ground Penetrating Radar (GPR) profiles, adding to a 40 km long walk across an Arctic glacier. The profiles were acquired using a Malå equipment with 100 MHz antennas, walking slowly enough to record a 2.224 µs trace every 30 cm on the average. Some acquisitions were repeated with 50 MHz or 200 MHz antenna to improve data quality. The GPR was coupled to a GPS system to position traces. Each profile has been manually edited using standard GPR data processing, to pick the reflection arrival time from the ice-bedrock interface. Travel-times were converted to ice thickness using a velocity of 0.17 m/ns. Dual-frequency GPS mapping and snow coverage thickness were acquired during the same survey. Using interpolation methods, we derived the underlying bedrock topography and evaluated the ice volume.
利用探地雷达对斯瓦尔巴群岛的奥斯特洛夫萨姆布林进行高密度覆盖调查
2010年4月,一项为期三周的实地调查获得了120个探地雷达(GPR)剖面,增加了穿越北极冰川40公里长的步行。这些轮廓是使用带有100 MHz天线的mal杆设备获得的,行走速度足够慢,平均每30厘米记录2.224µs的迹线。为了提高数据质量,使用50兆赫或200兆赫天线重复采集一些数据。探地雷达被连接到GPS系统来定位踪迹。每个剖面都使用标准GPR数据处理进行手动编辑,以从冰-基岩界面选择反射到达时间。以0.17米/秒的速度将行驶时间转换为冰厚。在同一次调查中获得了双频GPS测图和积雪厚度。利用插值方法,导出了下伏基岩地形,并对冰量进行了估算。
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