Preprints
https://doi.org/10.5194/egusphere-2025-3647
https://doi.org/10.5194/egusphere-2025-3647
26 Sep 2025
 | 26 Sep 2025
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Microstructure and ice dynamics – Integrating Grain Properties, Fabric, and Borehole Data in the NEEM Ice Core

Miguel Moreno, André Lamott, Sepp Kipfstuhl, Ilka Weikusat, María-Gema Llorens, Yannick Heiser, and Dorthe Dahl-Jensen

Abstract. The physical properties of ice grains, including grain size and orientation, are fundamental to understanding ice flow and deformation processes in polar ice sheets. This study leverages a newly developed large-area scanning microscope (xLASM) and an automated microtome to non-destructively analyze the NEEM ice core's microstructure across 55 cm segments. The resulting microstructural data are compared with continuous flow analysis (CFA) measurements of impurity concentrations, fabric orientation, and shear strain rates over a 16-meter section (2004–2020 m depth) that spans the Last Glacial Maximum and abrupt climatic transitions during Dansgaard-Oeschger event GS-20. Our results reveal strong associations between grain size, impurity concentrations, and shear deformation rates, with impurity-rich, fine-grained stadial ice exhibiting higher shear strain rates. The ice fabric remains stable despite the changes in shear deformation, indicating that, in this case, the fabric is not the cause of the changing deformation.

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Miguel Moreno, André Lamott, Sepp Kipfstuhl, Ilka Weikusat, María-Gema Llorens, Yannick Heiser, and Dorthe Dahl-Jensen

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Miguel Moreno, André Lamott, Sepp Kipfstuhl, Ilka Weikusat, María-Gema Llorens, Yannick Heiser, and Dorthe Dahl-Jensen
Miguel Moreno, André Lamott, Sepp Kipfstuhl, Ilka Weikusat, María-Gema Llorens, Yannick Heiser, and Dorthe Dahl-Jensen

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Short summary
By scanning a Greenland ice core, we studied the changes in ice flow. We found that during past rapid climate changes, the size of ice grains and the amount of impurities were the main factors controlling how the ice deformed. We found that other deep, structural properties of the ice did not change in the cores studied, suggesting they were not the primary cause of the variations in flow.
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