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A Wideband Direction of Arrival Technique for Multibeam, Wide-Swath Imaging of Ice Sheet Basal Morphology.

机译:冰层基础形态的多波束,宽幅成像的宽带到达技术方向。

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摘要

Multichannel, ice sounder data can be processed to three-dimensionally map ice sheet bed topography and basal reflectivity using tomographic imaging techniques. When ultra-wideband (UWB) signals are used to interrogate a glaciological target, fine resolution maps can be obtained. These data sets facilitate both process studies of ice sheet dynamics and also continental-scale ice sheet modeling needed to predict future sea level. The socioeconomic importance of these data as well as the cost and logistical challenge of procuring them justifies the need to image ice sheet basal morphology over a wider swath. Imaging wide swaths with UWB signals poses challenges for the array processing methods that have been used to localize scattering in the cross-track dimension. Both MUltiple SIgnal Classification (MUSIC) and the Maximum Likelihood Estimator (MLE) have been applied to the ice sheet tomography problem. These techniques are formulated assuming a narrowband model of the array that breaks down in wideband signal environments when the direction of arrival (DOA) increases further off nadir.;The Center for Remote Sensing of Ice Sheets (CReSIS) developed a UWB multichannel SAR with a large cross-track array for sounding and imaging polar ice from a Basler BT-67 aircraft. In 2013, this sensor collected data in a multibeam mode over the West Antarctic Ice Sheet to demonstrate wide swath imaging. To reliably estimate the arrival angles of echoes from the edges of the swath, a parametric space-time direction of arrival estimator was developed that obtains an estimate of the DOA by fitting the observed space-time covariance structure to a model. This thesis focuses on the development and optimization of the algorithm and describes its predicted performance based on simulation. Its measured performance is analyzed with 3D tomographic basal maps of an ice stream in West Antarctica that were generated using the technique.
机译:可以使用断层成像技术将多通道,测冰仪数据处理为三维冰盖床地形和基础反射率的三维地图。当使用超宽带(UWB)信号询问冰川目标时,可以获得高分辨率图。这些数据集既有助于冰盖动力学的过程研究,也有助于预测未来海平面所需的大陆规模冰盖建模。这些数据的社会经济重要性以及获得这些数据的成本和后勤挑战证明,有必要在更广泛的范围内对冰盖基础形态进行成像。用UWB信号对宽条带成像会给阵列处理方法带来挑战,这些方法已用于在跨轨道维度上定位散射。多重信号分类(MUSIC)和最大似然估计器(MLE)均已应用于冰盖层析成像问题。假设这些阵列的窄带模型在到达方向(DOA)远离最低点时会在宽带信号环境中破裂的情况下被公式化表示;冰原遥感中心(CReSIS)开发了一种UWB多通道SAR,具有大型跨轨阵列,用于探测和成像来自Basler BT-67飞机的极地冰。 2013年,该传感器以多波束模式在西南极冰原上收集了数据,以展示宽幅成像。为了可靠地估计来自条带边缘的回波的到达角,开发了参数时空到达方向估计器,该参数通过将观察到的时空协方差结构拟合到模型中来获得DOA的估计。本文重点研究了算法的开发和优化,并基于仿真描述了算法的预测性能。使用该技术生成的南极西部冰流的3D断层层析基础图分析了其测得的性能。

著录项

  • 作者

    Stumpf, Theresa.;

  • 作者单位

    University of Kansas.;

  • 授予单位 University of Kansas.;
  • 学科 Electrical engineering.
  • 学位 M.E.
  • 年度 2015
  • 页码 124 p.
  • 总页数 124
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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