Original Research ARTICLE
Radiostratigraphy reflects the present-day, internal ice flow field in the ablation zone of western Greenland
- 1Department of Geosciences, University of Montana, United States
- 2Department of Computer Sciences, University of Montana, United States
Englacial radar reflectors in the ablation zone of the Greenland Ice Sheet are derived from layering deposited in the accumulation zone over past millennia. The original layer structure is distorted by ice flow toward the margin. In a simplified case, shear and normal strain incurred between the ice divide and terminus should align depositional layers such that they closely approximate particle paths through the ablation zone where horizontal motion dominates. It is unclear, however, if this relationship holds in western Greenland where complex bed topography, three dimensional ice flow, and historical changes to ice sheet mass and geometry since layer deposition may promote a misalignment between present-day layer orientation and the modern ice flow field. We investigate this problem using a suite of analyses that leverage ice sheet models and observational datasets. Our findings suggest that across a study sector of western Greenland, the radiostratigraphy of the ablation zone is closely aligned with englacial particle paths, and is not far departed from a state of balance. The englacial radiostratigraphy thus provides insight into the modern, local, internal flow field, and may serve to further constrain ice sheet models that simulate ice dynamics in this region.
Keywords: Ice sheet dynamics, radiostratigraphy, Ice deformation, Ablation zone, Greenland ice sheet
Received: 08 Nov 2017;
Accepted: 11 Apr 2018.
Edited by:Alun Hubbard, UiT The Arctic University of Norway, Norway
Reviewed by:Andrew J. Sole, University of Sheffield, United Kingdom
Tom Holt, Aberystwyth University, United Kingdom
Joseph A. MacGregor, Goddard Space Flight Center, United States
Copyright: © 2018 Florentine, Harper, Johnson and Meierbachtol. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence: Ms. Caitlyn Florentine, University of Montana, Department of Geosciences, Missoula, United States, firstname.lastname@example.org