Fahrner Dominik, Slater Donald A, Kc Aman, Cenedese Claudia, Sutherland David A, Enderlin Ellyn, de Jong M Femke, Kjeldsen Kristian K, Wood Michael, Nienow Peter, Nowicki Sophie, Wagner Till J W
University of Oregon, Department of Earth Sciences, Eugene, OR, USA.
Geological Survey of Denmark and Greenland, Department of Glaciology and Climate, København, Denmark.
Sci Data. 2025 Apr 10;12(1):601. doi: 10.1038/s41597-025-04948-3.
Frontal ablation at tidewater glaciers, which comprises iceberg calving and submarine and subaerial melting, is a key boundary condition for numerical ice sheet models but remains difficult to measure in-situ. Although previous studies have provided frontal ablation estimates over a range of spatiotemporal scales, most use ice discharge as an approximation, thereby neglecting the influence of terminus position change. Here, we present a dataset of frontal ablation estimates for 49 tidewater glaciers in Greenland that have reliable near-terminus bathymetry data. Near-terminus volume change over the period 1987-2020 is determined using previously published datasets of terminus positions (TermPicks) together with ice thicknesses estimated from ArcticDEM, AeroDEM, and Bedmachine v5 bed topography. Assuming a vertical terminus geometry and uniform ice density, we estimate frontal ablation as the residual between mass flux towards the terminus taken from a published dataset and mass change due to changes in terminus position. The frontal ablation dataset offers opportunities for developing new insights into ice dynamics, including helping to improve numerical model hindcasting and projections.
在潮水冰川处的前沿消融,包括冰山崩解以及海底和陆面融化,是冰盖数值模型的一个关键边界条件,但现场测量仍很困难。尽管先前的研究已经在一系列时空尺度上提供了前沿消融估计值,但大多数研究将冰流量用作近似值,从而忽略了终点位置变化的影响。在此,我们展示了格陵兰49条拥有可靠近终点测深数据的潮水冰川的前沿消融估计数据集。利用先前发布的终点位置数据集(TermPicks)以及根据北极数字高程模型(ArcticDEM)、航空数字高程模型(AeroDEM)和Bedmachine v5床面地形估计的冰厚度,确定了1987年至2020年期间的近终点体积变化。假设终点为垂直几何形状且冰密度均匀,我们将前沿消融估计为已发布数据集中向终点的质量通量与终点位置变化导致的质量变化之间的差值。该前沿消融数据集为深入了解冰动力学提供了机会,包括有助于改进数值模型的后推和预测。