Large cracks in Antarctic ice shelves are regular occurrences driven by natural rift propagation
Large cracks and rifts in Antarctic ice shelves are regular occurrences driven by natural mechanical processes such as wave-induced stresses, shear deformation, and fracture mechanics.
The retrieved papers consistently describe large rifts and cracks in Antarctic ice shelves as natural features governed by physical processes like wave-induced stresses, internal structure heterogeneity, and shear stress along ice streams. No papers refute the natural occurrence and propagation mechanisms of these rifts.
Bradley Paul Lipovsky. Ice Shelf Rift Propagation and the Mechanics of Wave‐Induced Fracture. 2018. https://doi.org/10.1029/2017jc013664
Quantifies wave-induced natural stresses on ice shelf rifts to examine the mechanical basis of their propagation.
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Edward C. King, Jan De Rydt, G. Hilmar Gudmundsson. The internal structure of the Brunt Ice Shelf from ice-penetrating radar analysis and implications for ice shelf fracture. 2018. https://doi.org/10.5194/tc-2018-13
Shows how natural internal structures and stress fields dictate the rate and direction of rift propagation through ice shelves.
A. Humbert, D. Steinhage. The evolution of the western rift area of the Fimbul Ice Shelf, Antarctica. 2011. https://doi.org/10.5194/tcd-5-1089-2011
Analyzes how natural features like ice rumples and shear stress drive the formation and expansion of major rifts.
Bradley Lipovsky. Ice shelf rift propagation and the mechanics of wave-induced fracture. 2017. https://doi.org/10.31223/osf.io/a9vjb
Investigates the mechanics of wave-induced fracture and natural rift propagation dynamics on Antarctic ice shelves.
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