hdl:10013/epic.49137
Submarine glacial-landform distribution across the West Antarctic margin, from grounding line to slope: the Pine Island–Thwaites ice-stream system
Graham, AGC, Jakobsson, M, Nitsche, FO, Larter, RD, Anderson, JB, Hillenbrand, C-D, Gohl, K, Klages, JP, Smith, JA and Jenkins, A
;
Contact
Karsten.Gohl [ at ] awi.de
Abstract
Item Type
Article
Authors
Graham, AGC, Jakobsson, M, Nitsche, FO, Larter, RD, Anderson, JB, Hillenbrand, C-D, Gohl, K, Klages, JP, Smith, JA and Jenkins, A
;
Divisions
AWI Organizations > Geosciences > Geophysics
AWI Organizations > Geosciences > Marine Geology and Paleontology
AWI Organizations > Geosciences > Marine Geology and Paleontology
Primary Division
Programs
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.2: Earth system on tectonic time scales: From greenhouse to icehouse world
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.2: Earth system on tectonic time scales: From greenhouse to icehouse world
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Publication Status
Published
Eprint ID
42470
DOI
https://www.doi.org/10.1144/m46.173
Cite as
Graham, A.
,
Jakobsson, M.
,
Nitsche, F.
,
Larter, R.
,
Anderson, J.
,
Hillenbrand, C. D.
,
Gohl, K.
,
Klages, J.
,
Smith, J.
and
Jenkins, A.
(2016):
Submarine glacial-landform distribution across the West Antarctic margin, from grounding line to slope: the Pine Island–Thwaites ice-stream system
,
Geological Society, London, Memoirs,
46
(1),
pp. 493-500
.
doi: https://www.doi.org/10.1144/m46.173
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Campaigns
ANT > XXIII > 4
ANT > XXVI > 3
ANT > XXVI > 3
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