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Items: 5

1.

Physical analysis of an Antarctic ice core-towards an integration of micro- and macrodynamics of polar ice.

Weikusat I, Jansen D, Binder T, Eichler J, Faria SH, Wilhelms F, Kipfstuhl S, Sheldon S, Miller H, Dahl-Jensen D, Kleiner T.

Philos Trans A Math Phys Eng Sci. 2017 Feb 13;375(2086). pii: 20150347. doi: 10.1098/rsta.2015.0347.

2.

Dynamic recrystallization during deformation of polycrystalline ice: insights from numerical simulations.

Llorens MG, Griera A, Steinbach F, Bons PD, Gomez-Rivas E, Jansen D, Roessiger J, Lebensohn RA, Weikusat I.

Philos Trans A Math Phys Eng Sci. 2017 Feb 13;375(2086). pii: 20150346. doi: 10.1098/rsta.2015.0346.

PMID:
28025295
3.

Massive subsurface ice formed by refreezing of ice-shelf melt ponds.

Hubbard B, Luckman A, Ashmore DW, Bevan S, Kulessa B, Kuipers Munneke P, Philippe M, Jansen D, Booth A, Sevestre H, Tison JL, O'Leary M, Rutt I.

Nat Commun. 2016 Jun 10;7:11897. doi: 10.1038/ncomms11897.

4.

Converging flow and anisotropy cause large-scale folding in Greenland's ice sheet.

Bons PD, Jansen D, Mundel F, Bauer CC, Binder T, Eisen O, Jessell MW, Llorens MG, Steinbach F, Steinhage D, Weikusat I.

Nat Commun. 2016 Apr 29;7:11427. doi: 10.1038/ncomms11427.

5.

Marine ice regulates the future stability of a large Antarctic ice shelf.

Kulessa B, Jansen D, Luckman AJ, King EC, Sammonds PR.

Nat Commun. 2014 Apr 22;5:3707. doi: 10.1038/ncomms4707.

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