A MFP-plus-relocation workflow localizes surface icequakes on Hansbreen, producing crevasse propagation rates and diffusion coefficients of 0.47-0.55 m²/s interpreted as sustained subcritical crack propagation.
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Surface Crevasse Evolution Observed Using Matched Field Processing and Source Relocation at Hansbreen, Svalbard
A MFP-plus-relocation workflow localizes surface icequakes on Hansbreen, producing crevasse propagation rates and diffusion coefficients of 0.47-0.55 m²/s interpreted as sustained subcritical crack propagation.