4.7 Article

Co-seismic eruption and intermittent turbulence of a subglacial discharge plume revealed by continuous subsurface observations in Greenland

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Summary: Ice mass loss from the Greenland ice sheet, mainly due to thinning and retreat of outlet glaciers, is the largest single contributor to sea level rise in the 21st century. Understanding the diverse calving mechanisms of tidewater glaciers is necessary to improve projections of ice sheet mass loss by calving. Recent observations suggest a change towards buoyant calving at Bowdoin Glacier, highlighting the need for high-resolution monitoring and numerical models to detect changing calving styles and improve projections of ice sheet mass loss by calving.

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