Ambient seismic noise under the sea-ice of the Arctic Ocean: First results from a pilot experiment with Ocean Bottom Seismometers at eastern Gakkel Ridge
Seismic monitoring of the cryosphere is mostly done with land seismometers on the surface of ice masses. Seismic monitoring beneath sea ice at the bottom of ice-covered oceans has hardly been attempted, because ocean bottom seismometers (OBS) are difficult to recover in perennial sea ice. As a resul...
Main Authors: | , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2021
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/54934/ https://hdl.handle.net/10013/epic.eff01915-fdab-4ae5-83b3-d4712bb8a160 |