Hidden cascades of seismic ice stream deformation

Ice streams are major regulators of sea level change. However, standard viscous flow simulations of their evolution have limited predictive power owing to incomplete understanding of involved processes. On the Greenland ice sheet, borehole fiber-optic observations revealed a brittle deformation mode that is incompatible with viscous flow, over length scales similar to the resolution of modern ice sheet models: englacial ice quake cascades that are unobservable at the surface. Nucleating near volcanism-related impurities that promote grain boundary cracking, the ice quake cascades appear as a macroscopic form of crystal-scale wild plasticity. A conservative estimate indicates that seismic cascades are likely to produce strain rates that are comparable in amplitude with those measured geodetically, providing a plausible missing link between current ice sheet models and observations.

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Publication Details

Journal
Science
Published
2025-02-06
DOI
https://doi.org/10.1126/science.adp8094
Citations
14
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
18.21
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article

Hidden cascades of seismic ice stream deformation

Daniela Jansen, Julien Westhoff, Andreas Fichtner, Fabian Walter et al.
14 citations
Science
Cryospheric studies and observations
18.21
article

Hidden cascades of seismic ice stream deformation

Daniela Jansen, Julien Westhoff, Andreas Fichtner, Fabian Walter, Coen Hofstede, Anders Svensson, Eliza Cook, Olaf Eisen, Jean‐Paul Ampuero, Dimitri Zigone, B. L. N. Kennett
article en
14 citations

Abstract

Ice streams are major regulators of sea level change. However, standard viscous flow simulations of their evolution have limited predictive power owing to incomplete understanding of involved processes. On the Greenland ice sheet, borehole fiber-optic observations revealed a brittle deformation mode that is incompatible with viscous flow, over length scales similar to the resolution of modern ice sheet models: englacial ice quake cascades that are unobservable at the surface. Nucleating near volcanism-related impurities that promote grain boundary cracking, the ice quake cascades appear as a macroscopic form of crystal-scale wild plasticity. A conservative estimate indicates that seismic cascades are likely to produce strain rates that are comparable in amplitude with those measured geodetically, providing a plausible missing link between current ice sheet models and observations.

ScienceVol. 387(6736)
Australian National University (AU), University of Copenhagen (DK), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Centre National de la Recherche Scientifique (FR), University of Bremen (DE), Swiss Federal Institute for Forest, Snow and Landscape Research (CH), ETH Zurich (CH), Observatoire de la Côte d’Azur (FR), Institut de Recherche pour le Développement (FR), Université de Strasbourg (FR)
Life below water
Openalex Percentile: Top 0%
Cryospheric studies and observations
18.21
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