The periodic topography of ice stream beds: Insights from the Fourier spectra of mega‐scale glacial lineations. Issue 7 (15th July 2017)

• Record Type: Journal Article
• Authors: Spagnolo, Matteo; Bartholomaus, Timothy C.; Clark, Chris D.; Stokes, Chris R.; Atkinson, Nigel; Dowdeswell, Julian A.; Ely, Jeremy C.; Graham, Alastair G. C.; Hogan, Kelly A.; King, Edward C.; Larter, Robert D.; Livingstone, Stephen J.; Pritchard, Hamish D.
• Is Part Of: Journal of geophysical research. Volume 122:Issue 7(2017)
• Page Start: 1355
• Page End: 1373
• Publication Date: 2017-07-15
• Subjects: ice stream bed -- mega‐scale glacial lineations -- period topography -- pattern topography -- Fourier; Geomorphology -- Periodicals; 551.3
• DOI: 10.1002/2016JF004154
• Languages: English
• ISSNs: 2169-9003

Abstract

Abstract: Ice stream bed topography contains key evidence for the ways ice streams interact with, and are potentially controlled by, their beds. Here we present the first application of two‐dimensional Fourier analysis to 22 marine and terrestrial topographies from 5 regions in Antarctica and Canada, with and without mega‐scale glacial lineations (MSGLs). We find that the topography of MSGL‐rich ice stream sedimentary beds is characterized by multiple, periodic wavelengths between 300 and 1200 m and amplitudes from decimeters to a few meters. This periodic topography is consistent with the idea that instability is a key element to the formation of MSGL bedforms. Dominant wavelengths vary among locations and, on one paleo ice stream bed, increase along the direction of ice flow by 1.7 ± 0.52% km −1 . We suggest that these changes are likely to reflect pattern evolution via downstream wavelength coarsening, even under potentially steady ice stream geometry and flow conditions. The amplitude of MSGLs is smaller than that of other fluvial and glacial topographies but within the same order of magnitude. However, MSGLs are a striking component of ice stream beds because the topographic amplitude of features not aligned with ice flow is reduced by an order of magnitude relative to those oriented with the flow direction. This study represents the first attempt to automatically derive the spectral signatures of MSGLs. It highlights the plausibility of identifying these landform assemblages using automated techniques and provides a benchmark for numerical models of ice stream flow and subglacial landscape evolution. Key Points: MSGL topography consists of superimposed periodic wavelengths as expected in the instability theory of subglacial bedform formation Most of the dominant wavelengths present within one extensive MSGL field increase downstream, suggesting that MSGLs evolve via pattern coarsening For MSGLs to generate periodic topography, sediment must be able to accumulate or erode (freely move) without fixed anchor points