EGU2020-6042
https://doi.org/10.5194/egusphere-egu2020-6042
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Constraints on glacier bedrock roughness from spectral analysis of glacier forefields

Jacob Woodard1, Lucas Zoet1, Neal Iverson2, and Christian Helanow2
Jacob Woodard et al.
  • 1University of Wisconsin-Madison, Department of Geoscience, Madison, United States of America (jwoodard2@wisc.edu)
  • 2Iowa State University of Science and Technology, Department of Geological and Atmospheric Sciences, Ames, United States of America

The slip of hard bedded glaciers partly depends on the morphology of their beds. Thus, constraints on subglacial bedrock morphology are imperative for accurate forecasting of glacier flow rates. Digital elevation models (DEMs) from ten valley glacier and ice-sheet forefields were used to analyze the spectral patterns of recently deglaciated bedrock. Valley glacier DEM length scales are 0.1 m - 100 m, while ice sheet DEM length scales are 10 m -1000 m. We observe a higher spectral roughness and aspect ratio (i.e. bump height/wavelength) for valley glaciers than ice-sheet forefields. However, forefield aspect ratios span a narrow range and decrease with increasing length scale at a consistent rate despite a range of bedrock lithologies analyzed. This implies that bedrock shear strength (τ) scales with length scale (L), as τ ~ L-0.37, closely matching the bulk strength scaling relation seen in fault rocks (Brodsky et al., 2016). These morphological constraints of forefields allow extrapolation of bedrock roughness beneath active glaciers that can help predict sliding rates.

How to cite: Woodard, J., Zoet, L., Iverson, N., and Helanow, C.: Constraints on glacier bedrock roughness from spectral analysis of glacier forefields , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6042, https://doi.org/10.5194/egusphere-egu2020-6042, 2020

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