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Volume 644 Issue 8076, 14 August 2025
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Volume 644 Issue 8076, 14 August 2025

Troubled waters

Glacier calving — when ice chunks break away to form icebergs — combined with underwater melting is the main driver for loss of mass from the Greenland Ice Sheet, but the detailed dynamics of this process have remained elusive. In this week’s issue, Dominik Gräff and colleagues use fibre-optic sensing to provide a picture of the complex effects of iceberg formation. The researchers found that as icebergs detach from the parent glacier, they spark a series of interactions — including tsunamis and internal waves — that amplify underwater melting and probably lead to further increases in calving. The cover picture captures the face of a Greenland iceberg that resembles the calving front of a glacier with ice fractures and calving-induced tsunamis undercutting the ice front.

Cover image: Richard Mardens.

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