Zusammenfassung
Reliable knowledge of ice discharge dynamics for the Greenland ice sheet via its ice streams is essential if we are to understand its stability under future climate scenarios as well as their dynamics in the past. Currently, active ice streams in Greenland have been well mapped using remote-sensing data while past ice-stream paths in what are now deglaciated regions can be reconstructed from the landforms they left behind. However, little is known about possible former and now defunct ice streams in areas still covered by ice. Here, we use radio-echo sounding data to decipher the regional ice-flow history of the northeastern Greenland ice sheet on the basis of its internal stratigraphy. Based on the same data set we also establish age-depth distributions in the ice stream and determine the physical properties of the ice, notably the distribution of anisotropy. By creating a three-dimensional reconstruction of time-equivalent horizons, we map folds deep below the surface that we then attribute to the deformation caused by now-extinct ice streams. We propose that locally this ancient ice-flow regime was much more focused and reached much farther inland than today’s and was deactivated when the main drainage system was reconfigured and relocated southwards. The insight that major ice streams in Greenland might start, shift or abruptly disappear will affect future approaches to understanding and modelling the response of Earth’s ice sheets to global warming.
EGRIP radar consortium: Daniela Jansen, Steven Franke, Tobias Binder, Paul D. Bons, Dorthe Dahl-Jensen, Reinhard Drews, Graeme Eagles, Olaf Eisen, Reza Ershadi, Tamara Annina Gerber, Prasad Gogineni, Aslak Grinsted, Veit Helm, Angelika Humbert, Christine Hvidberg, David Lilien, Heinrich Miller, Charles O'Neill, John D. Paden, Nicholas Rathmann, Daniel Steinhage, Nicolas Stoll, Kyra Streng, Fernando Valero-Delgado, Ilka Weikusat, Julien Westhoff, Tun Jan Young, Ole Zeising
