Subglacial sediment pathways and deglacial chronology of the northern Barents Sea Ice Sheet

Author:

Hogan Kelly A.1ORCID,Dowdeswell Julian A.2,Hillenbrand Claus-Dieter1,Ehrmann Werner3,Noormets Riko4,Wacker Lukas5

Affiliation:

1. British Antarctic Survey; NERC; High Cross, Madingley Road Cambridge CB3 0ET UK

2. Scott Polar Research Institute; University of Cambridge; Lensfield Road Cambridge CB2 1ER UK

3. Institute of Geophysics and Geology; University of Leipzig; Talstraße 35 Leipzig D-04103 Germany

4. University Centre on Svalbard; UNIS; Longyearbyen Norway

5. Ion Beam Physics; ETH Zurich; Zurich 8093 Switzerland

Funder

Iain Hiller Award Scheme

Natural Environment Research Council

Publisher

Wiley

Subject

Geology,Archaeology,Ecology, Evolution, Behavior and Systematics

Reference103 articles.

1. Aagaard-Sørensen , S. Groot , D. E. Husum , K. Hald , M. 2013 Paleoceanographic reconstruction in the western and northern Barents Sea during and after the last deglaciation EGU General Assembly Conference Abstracts, EGU2013-2766

2. Outlet glacier and margin elevation changes: near-coastal thinning of the Greenland ice sheet;Abdalati;Journal of Geophysical Research: Atmospheres,2001

3. Late quaternary sedimentation and glacial history of the western Svalbard continental margin;Andersen;Marine Geology,1996

4. Landform assemblage from the collapse of the Bjørnøyrenna palaeo-ice stream, northern Barents Sea;Andreassen;Quaternary Science Reviews,2014

5. Glacial isostatic adjustment associated with the Barents Sea ice sheet: a modelling inter-comparison;Auriac;Quaternary Science Reviews,2016

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