Seismic evidence for complex sedimentary control of Greenland Ice Sheet flow

Author:

Kulessa Bernd1,Hubbard Alun L.23,Booth Adam D.4,Bougamont Marion5,Dow Christine F.6,Doyle Samuel H.3,Christoffersen Poul5ORCID,Lindbäck Katrin7,Pettersson Rickard8,Fitzpatrick Andrew A. W.3,Jones Glenn A.13

Affiliation:

1. Glaciology Group, College of Science, Swansea University, Singleton Park, Swansea SA2 8PP, UK.

2. Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, 9037 Tromsø, Norway.

3. Centre for Glaciology, Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth SY23 3DB, UK.

4. Institute of Applied Geoscience, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK.

5. Scott Polar Research Institute, Department of Geography, University of Cambridge, Cambridge CB2 1ER, UK.

6. Department of Geography and Environmental Management, University of Waterloo, 200 University Avenue West, Waterloo, Ontario N2L 3G1, Canada.

7. Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway.

8. Department of Earth Sciences, Uppsala Universitet, Villavägen 16, 752 36 Uppsala, Sweden.

Abstract

Seismic data show that subglacial sediment slip causes a complex flow response of the Greenland Ice Sheet to climate warming.

Funder

Natural Environment Research Council

Forskningsradet, Norway

SKB Posiva NWMO

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference58 articles.

1. N. L. Bindoff P. A. Stott K. M. AchutaRao M. Allen N. Gillett D. Gutzler K. Hansingo G. Hegerl Y. Hu S. Jain I. Mokhov J. Overland J. Perlwitz R. Sebbari X. Zhang Detection and attribution of climate change: From global to regional in Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change T. F. Stocker D. Qin G.-K. Plattner M. Tignor S. K. Allen J. Boschung A. Nauels Y. Xia V. Bex P. M. Midgley Eds. (Cambridge Univ. Press 2013) pp. 867–952.

2. Enhanced basal lubrication and the contribution of the Greenland ice sheet to future sea-level rise;Shannon S. R.;Proc. Natl. Acad. Sci. U.S.A.,2013

3. Sensitive response of the Greenland Ice Sheet to surface melt drainage over a soft bed

4. Surface Melt-Induced Acceleration of Greenland Ice-Sheet Flow

5. Greenland ice sheet motion coupled with daily melting in late summer;Shepherd A.;Geophys. Res. Lett.,2009

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