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Subglacial landforms beneath Rutford Ice Stream, Antarctica: detailed bed topography from ice-penetrating radar

机译:南极拉特福德冰河下面的冰下地貌:穿透冰雷达的详细河床地形

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We present a digital elevation model of the bed of Rutford Ice Stream, Antarctica, derived from radio-echo sounding data. The data cover an 18??×??40?km area immediately upstream of the grounding line of the ice stream. This area is of particular interest because repeated seismic surveys have shown that rapid erosion and deposition of subglacial sediments has taken place. The bed topography shows a range of different subglacial landforms including mega-scale glacial lineations, drumlins and hummocks. This data set will form a baseline survey which, when compared to future surveys, should reveal how active subglacial landscapes change over time. These data also allow comparison between subglacial landforms in an active system with those observed in deglaciated areas in both polar regions. The data set comprises observed ice thickness data, an interpolated bed elevation grid, observed surface elevation data and a surface elevation grid. The data set is available at http://doi.org/269.
机译:我们介绍了南极拉特福德冰河床的数字高程模型,该模型是根据无线电回声测深数据得出的。数据覆盖了冰流接地线上游的一个18×40×40 km的区域。该地区特别受关注,因为反复进行的地震调查表明,冰川下沉积物已经发生了快速侵蚀和沉积。床的地形显示了一系列不同的亚冰川地貌,包括大型冰川系,鼓林和山岗。该数据集将构成基线调查,与将来的调查相比,该调查应揭示活跃的冰川下景观如何随时间变化。这些数据还可以将活跃系统中的冰下地貌与两个极地冰川地区的观测结果进行比较。该数据集包括观测到的冰厚数据,内插床层高程网格,观测到的表面高程数据和表面高程网格。该数据集可从http://doi.org/269获得。

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