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Ice-stream demise dynamically conditioned by trough shape and bed strength
Tom Bradwell1,2, David Small3, Derek Fabel4
1Biological and Environmental Sciences, University of Stirling, Stirling FK9 4LA, UK.
Science Advances
|May 7, 2019
Summary
Glacial ice stream retreat was significantly influenced by bed strength and trough shape, not just external factors. A transition from weak to strong beds around 18,500 years ago triggered rapid ice-stream demise.
Area of Science:
- * Glaciology and Paleoclimatology
- * Ice Sheet Dynamics
Background:
- * Ice sheet mass loss is primarily driven by fast-flowing glaciers (ice streams) that terminate in the ocean.
- * Understanding long-term ice-stream flow, retreat, and the influence of bed topography and strength is crucial for predicting future ice loss.
Purpose of the Study:
- * To reconstruct the retreat history and grounding-line movements of a former ice stream over the past 15,000 years.
- * To investigate the role of geological factors, specifically bed shape and substrate, in controlling ice-stream behavior.
Main Methods:
- * Analysis of a former ice stream with known or definable trough geometry and bed substrate.
- * Reconstruction of ice-stream retreat and grounding-line migration since the Last Glacial Maximum.
Main Results:
- * A significant behavioral shift in ice-stream retreat occurred between 18,500 and 16,000 years ago.
- * This shift, independent of external forcing, correlated with the collapse of floating ice sectors and rapid ice-front retreat.
- * The event was linked to a geological transition from a soft/weak bed to a hard/strong bed, coupled with changes in trough geometry.
Conclusions:
- * Geological factors, including bed strength and trough shape, played a critical role in the demise of the studied ice stream.
- * These factors conditioned and accelerated ice-stream retreat, highlighting their importance in past and potentially future ice sheet behavior.
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