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BedMachine v3 : complete bed topography and ocean bathymetry mapping of Greenland from multibeam echo sounding combined with mass conservation.

机译:BedMachine v3:通过多波束回波测深结合质量守恒来完成格陵兰的完整河床地形图和海洋测深图。

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摘要

Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the penetration of warm Atlantic water (AW) that rapidly melts and undercuts Greenland's marine-terminating glaciers. Here we present a new compilation of Greenland bed topography that assimilates seafloor bathymetry and ice thickness data through a mass conservation approach. A new 150 m horizontal resolution bed topography/bathymetric map of Greenland is constructed with seamless transitions at the ice/ocean interface, yielding major improvements over previous data sets, particularly in the marine-terminating sectors of northwest and southeast Greenland. Our map reveals that the total sea level potential of the Greenland ice sheet is 7.42 ± 0.05 m, which is 7 cm greater than previous estimates. Furthermore, it explains recent calving front response of numerous outlet glaciers and reveals new pathways by which AW can access glaciers with marine-based basins, thereby highlighting sectors of Greenland that are most vulnerable to future oceanic forcing.
机译:格陵兰的河床地形是对冰流量,地线迁移,产犊动态和冰川下排水的主要控制。此外,峡湾测深仪还调节着大西洋的温暖水(AW)的渗透,迅速融化并削弱了格陵兰岛海洋终结的冰川。在这里,我们介绍了格陵兰河床地形的新汇编,它通过质量守恒方法吸收了海底测深和冰厚数据。构造了新的150微米水平分辨率的格陵兰河床地形/测深图,并在冰/海界面处进行了无缝过渡,与以前的数据集相比有了重大改进,尤其是在格陵兰西北部和东南部的海洋终止地区。我们的地图显示格陵兰冰盖的总海平面潜力为7.42±0.05 m,比以前的估计值大7厘米。此外,它解释了近期众多出口冰川的前倾反应,并揭示了AW可以利用海洋盆地进入冰川的新途径,从而突出了格陵兰最容易受到未来海洋强迫作用的部分。

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