Nature Communications (May 2018)
The Holocene retreat dynamics and stability of Petermann Glacier in northwest Greenland
Abstract
Submarine glacial landforms are used to reconstruct the Holocene retreat dynamics and stability of Petermann Glacier in northwest Greenland. Here, a large grounding-zone wedge at the mouth of Petermann fjord indicates a period of glacier stability, with final retreat likely driven by marine ice cliff instability.