The Physics of Ice Shelf Calving: How Flexural Stress and Hydrofracture Interact at Glacial Margins
冰架崩解的物理学:弯曲应力与水力劈裂在冰川边缘的相互作用
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Ice shelves resist inland glacier flow by transmitting buttressing stresses across their width—calving events compromise this mechanical restraint.
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Flexural stress arises from differential flow velocities across the shelf, inducing tensile strain at the upper surface near grounding lines.
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