Key advantages of deploying an ocean-bottom seismometer near the calving front of a tidewater glacier (IMAGE)
Caption
Key advantages of deploying an ocean-bottom seismometer near the calving front of a tidewater glacier. Subglacial and ocean seismo-acoustic signals can be detected, while the impact of surface seismic sources is minimised (Evgeny A. Podolskiy, Yoshio Murai, Naoya Kanna, Shin Sugiyama. Nature Communications. June 24, 2021).
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Evgeny A. Podolskiy, Yoshio Murai, Naoya Kanna, Shin Sugiyama. Nature Communications. June 24, 2021
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