Geophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciation-Reference-Cited by-同舟云学术

Geophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciation

Published:2015-11-14 Issue:4 Volume:53 Page:1051-1098
ISSN:8755-1209
Container-title:Reviews of Geophysics
language:en
Short-container-title:Rev. Geophys.

Author:

Patton Henry¹^ORCID,Andreassen Karin¹,Bjarnadóttir Lilja R.²,Dowdeswell Julian A.³,Winsborrow Monica C. M.¹,Noormets Riko⁴,Polyak Leonid¹⁵,Auriac Amandine⁶,Hubbard Alun¹

Affiliation:

1. CAGE-Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geology; UiT The Arctic University of Norway; Tromsø Norway

2. Geological Survey of Norway; Trondheim Norway

3. Scott Polar Research Institute; University of Cambridge; Cambridge UK

4. University Centre in Svalbard (UNIS); Longyearbyen Norway

5. Byrd Polar Research Center; Ohio State University; Columbus Ohio USA

6. Department of Geography; Durham University; Durham UK

Funder

“Glaciations in the Barents Sea area” (GlaciBar)

Centres of Excellence

Publisher

American Geophysical Union (AGU)

Subject

Geophysics

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