Research results

Tide-modulated ice flow variations drive seismicity near the calving front of Bowdoin Glacier, Greenland.

Podolskiy, E.A., S. Sugiyama, M. Funk, F. Walter, R. Genco, S. Tsutaki, M. Minowa, and M. Ripepe (2016). Tide-modulated ice flow variations drive seismicity near the calving front of Bowdoin Glacier, Greenland. Geophysical Research Letters, 43, 2036–2044

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