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BedMachine v3: Complete bed topography and ocean bathymetry mapping of Greenland from multi-beam echo sounding combined with mass conservation

机译:Bedmachine v3:格陵兰从多波束回波探测到质量守恒的完整床地形和海洋测深测绘

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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 (MC) 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 datasets, particularly in the marine-terminating sectors of northwest and southeast Greenland. Our map reveals 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冰流,地线迁移,产犊动态和冰川下排水的主要控制因素。此外,峡湾测深仪还调节着温暖的大西洋水(AW)的渗透,该融化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,该汇编通过质量守恒(MC)方法吸收了海底测深和冰厚数据。构建了新的150 m格陵兰岛水平分辨率河床地形/测深图,在冰/海界面处进行了无缝过渡,与以前的数据集相比,尤其是在格陵兰岛西北部和东南部的海洋终端地区,有了重大改进。我们的地图显示格陵兰冰原的总海平面潜力为7.42±0.05 m,比先前的估计值高7 cm。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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