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A wideband radar for mapping internal layers in the polar icesheets for estimating accumulation rate

机译:用于在极地ICESHEET中映射内部层的宽带雷达,以估计累积率

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Determination of the mass balance of the polar ice sheets requires information on the accumulation rate. Remote sensing methods to determine the accumulation rate are essential in reducing the uncertainty associated with interpolating in situ measurements that are obtained from ice cores and pits. This is essential to reducing the 20% of uncertainty in current accumulation rate maps. Using data from surface-based radar experiments we determined optimum parameters for an airborne radar. We developed an airborne prototype and successfully demonstrated that we can map internal layers with about 1 m resolution to a depth of about 120 m over the Greenland ice sheet. We reported the system design, construction and preliminary experimental results at the 2001 IGARSS meeting. We have developed an operational radar system for routine measurement. This system operates in FM-CW and stepped-frequency pulse modes and it has 20-dB more sensitivity than the prototype radar. We also developed a radar target simulator for testing and evaluating system performance. The target simulator was constructed using fiber optic cables, microwave delay lines and RF/optical transceivers to simulate reflections from the air/snow interface, internal layers and the antenna reflection, which degrades the system's sensitivity. The simulator serves a dual purpose of optimizing the system performance in the laboratory and for internal calibration in the field. We also used a CAD package to design and simulate overall radar performance. The use of CAD package and target simulator reduced cost and time associated with the radar development. In addition, we are also able to obtain an accurate system model to deconvolve the system effects from the received signal. We discuss detailed design, construction and performance of the target simulator and operational radar. We show a comparison of the simulation results and laboratory measurements of the radar system. Also we present analysis of the results from measurements made during the 2001 experiments and preliminary results from planned measurements in May 2002.
机译:极性冰盖的质量平衡的测定需要有关累积率的信息。用于确定累积率的遥感方法对于减少与从冰芯和凹坑获得的原位测量的内插相关相关的不确定性是必要的。这对于减少当前累积率图中的20%的不确定性至关重要。使用来自基于表面的雷达实验的数据我们确定了空降雷达的最佳参数。我们开发了一个空中原型,并成功地证明了我们可以将大约1米分辨率的内部层映射到格陵兰冰板约120米的深度。我们报告了2001年IGARS会议的系统设计,建设和初步实验结果。我们开发了一个用于常规测量的操作雷达系统。该系统以FM-CW和阶梯式脉冲模式操作,它具有比原型雷达更高的灵敏度20-DB。我们还开发了一种雷达目标模拟器,用于测试和评估系统性能。使用光纤电缆,微波延迟线和射频/光收发器构造目标模拟器,以模拟空气/积雪,内部层和天线反射的反射,这会降低系统的灵敏度。该模拟器有助于优化实验室中的系统性能和现场内部校准的双重目的。我们还使用CAD包来设计和模拟整体雷达性能。使用CAD包和目标模拟器降低了与雷达开发相关的成本和时间。此外,我们还能够获得精确的系统模型来解码来自接收信号的系统效应。我们讨论了目标模拟器和操作雷达的详细设计,构建和性能。我们展示了雷达系统的仿真结果和实验室测量的比较。此外,我们对2001年5月在2001年5月的计划测量中进行了测量结果的分析。

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