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Investigation of Tandem-x Penetration Depth Over the Greenland Ice Sheet

机译:格陵兰冰盖上纵列-x穿透深度的研究

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Ongoing global warming causes dramatic changes globally, especially with respect to Polar Regions. In this context, digital elevation data is of high importance for most glaciological applications. In this paper, we investigate TanDEM-X penetration depth over snow and ice on the Greenland ice sheet. In particular, the relation of backscatter intensity and interferometric coherence to penetration depth of the X-band InSAR signal is explored in order to improve the reliability of TanDEM-X elevation data. The analyses showed a distinct relationship of backscatter intensity, coherence and penetration depth. In addition, the influence of the height of ambiguity of the interferometric TanDEM-X data is presented. On an experimental test site in Northern Greenland, we demonstrated the estimation of TanDEM-X penetration depth based on backscatter intensity and interferometric coherence utilizing a linear regression model.
机译:持续的全球变暖在全球范围内引起了巨大变化,特别是在极地地区。在这种情况下,数字高程数据对于大多数冰川学应用而言至关重要。在本文中,我们研究了TanDEM-X在格陵兰冰原上在冰雪上的穿透深度。特别地,探索了反向散射强度和干涉相干性与X波段InSAR信号的穿透深度之间的关系,以提高TanDEM-X仰角数据的可靠性。分析表明反向散射强度,相干性和穿透深度之间存在明显的关系。此外,还介绍了干涉式TanDEM-X数据歧义高度的影响。在格陵兰北部的一个实验测试现场,我们证明了使用线性回归模型基于反向散射强度和干涉相干性估算TanDEM-X的穿透深度。

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