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Numerical simulations of drumlin formation.

J S Fannon1, A C Fowler1,2, I R Moyles1

  • 1MACSI, University of Limerick, Limerick, Ireland.

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|September 8, 2017
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Summary
This summary is machine-generated.

The instability theory for drumlin formation now predicts glacial landforms like drumlins and mega-scale glacial lineations. A new numerical method solves this complex subglacial process, revealing realistic bedform evolution.

Keywords:
drumlinsinstabilitymega-scale glacial lineationsribbed moraine

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Area of Science:

  • Glaciology
  • Geomorphology
  • Sedimentology

Background:

  • The instability theory for drumlin formation models coupled subglacial processes involving ice, water, and sediment.
  • This theory has evolved over two decades, enabling predictions of various glacial landforms, including ribbed moraines, drumlins, and mega-scale glacial lineations.
  • Previous efforts to numerically solve the model have been constrained.

Purpose of the Study:

  • To present the current state of the drumlin formation instability theory.
  • To introduce a novel numerical method for solving the model.
  • To investigate the model's ability to simulate realistic glacial bedform evolution.

Main Methods:

  • Summarizing and refining the existing instability theory for drumlin formation.
  • Developing a new numerical approach to solve the coupled subglacial flow model.
  • Testing the model with realistic parameter values, focusing on the subglacial water film.

Main Results:

  • The refined theory incorporates updated descriptions of the subglacial water film and its flow.
  • The new numerical method allows for solutions with most parameters set to realistic values, except for water film thickness.
  • The model successfully generates three-dimensional bedforms of appropriate sizes, demonstrating sensitivity to parameter variations.

Conclusions:

  • The instability theory provides a robust framework for understanding drumlin formation and related glacial landforms.
  • The developed numerical method enhances the model's solvability for realistic glacial conditions.
  • Further research is needed to refine the representation of subglacial water film thickness for even more accurate simulations.