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New ice thickness maps of Filchner-Ronne Ice Shelf, Antarctica, with specific focus on grounding lines and marine ice

机译:南极Filchner-Ronne冰架的新冰厚度图,特别关注接地线和海冰

摘要

For the Filchner-Ronne Ice Shelf we have compiled measurements of meteoric ice thickness from many institutions, and several different techniques (e.g. radar and seismic sounding) to produce an improved digital map of meteoric ice thickness. This map has high-resolution compared to previous compilations and serves to highlight small-scale geographic features (e.g. ice plains, grounding-line regions). We have also produced a map of the thickness of marine ice bodies beneath the ice shelf by using borehole density data to calibrate an ice thickness to surface-elevation relation, and then comparing maps of ice surface elevation and meteoric ice thickness to infer marine ice thickness. Due to denser data coverage and the improved density-depth relation, the resulting map is a significant improvement on its predecessors and allows insight into the glaciological context of the ice shelf, in particular, into the location of the grounding lines on the southern Ronne Ice Shelf. Here the data were supplemented with barometric determination of surface elevation, which were used to locate the grounding line position. The final delineation of the grounding line position was confirmed by reference to satellite imagery, and revealed that earlier estimates were substantially in error, especially in the area of Foundation Ice Stream and Mollereisstrom.
机译:对于Filchner-Ronne冰架,我们已经汇编了许多机构对陨石冰厚的测量结果,并采用了几种不同的技术(例如雷达和地震测深仪)以生成改进的陨石冰厚数字地图。与以前的版本相比,该地图具有高分辨率,并且可以突出显示小规模的地理特征(例如,冰原,地线区域)。我们还使用井眼密度数据校准了冰层厚度与地表高程的关系,然后比较了冰面高度和流星冰层厚度的地图以推断出海洋冰层厚度,从而绘制了冰架下方海洋冰体厚度的地图。 。由于更密集的数据覆盖和改进的密度-深度关系,所生成的地图是其前身的重大改进,可以洞察冰架的冰川环境,尤其是Ronne Ice南部的地线位置架。在此,对数据进行了地面高度的气压测定,以用于确定接地线的位置。参照卫星图像确认了接地线位置的最终划定,并揭示了先前的估计是相当错误的,尤其是在基金会冰河和Mollereisstrom地区。

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