Subglacial landscape in the Antarctic interior consistent with past fast ice flow
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://www.nature.com/articles/s41561-023-01267-3.pdf
Reference6 articles.
1. Paden, J., Akins, T., Dunson, D., Allen, C. & Gogineni, P. Ice-sheet bed 3-D tomography. J. Glaciol. 56, 3–11 (2010). An early report of the application of swath radar technology to ice sheets.
2. Spagnolo, M. et al. The periodic topography of ice stream beds: insights from Fourier spectra of mega-scale glacial lineations. J. Geophys. Res. Earth Surf. 122, 1355–1373 (2017). This paper reports on connections between landform geometry and ice flow speed.
3. Robel, A. A., Roe, G. H. & Haseloff, M. Response of marine-terminating glaciers to forcing: time scales, sensitivity, instabilities, and stochastic dynamics. J. Geophys. Res. Earth Surf. 123, 2205–2227 (2018). This study reports the use of reduced modelling to elucidate the ice-stream response to forcing.
4. Winter, K. et al. Topographic steering of enhanced ice flow at the bottleneck of between East and West Antarctica. Geophys. Res. Lett. 45, 4899–4907 (2018). This paper presents aerogeophysical data indicating ice flow is steered by large topographic basins in central Antarctica.
5. Morlighem, M. et al. Deep glacial troughs and stabilizing ridges beneath the margins of the Antarctic ice sheet. Nat. Geosci. 13, 132–137 (2020). This paper presents the application of mass conservation modelling to map the topography of the Antarctic bed.
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