Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH Hellmer, F Kauker, R Timmermann, J Determann… - Nature, 2012 - nature.com
The Antarctic ice sheet loses mass at its fringes bordering the Southern Ocean. At this
boundary, warm circumpolar water can override the continental slope front, reaching the …
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[引用][C] Twenty―first―century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH HELLMER, F KAUKER, R TIMMERMANN… - Nature …, 2012 - pascal-francis.inist.fr
Twenty―first―century warming of a large Antarctic ice-shelf cavity by a redirected coastal
current CNRS Inist Pascal-Francis CNRS Pascal and Francis Bibliographic Databases …

[引用][C] Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH Hellmer - (No Title), 2012 - cir.nii.ac.jp
Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current
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Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH Hellmer, F Kauker, R Timmermann, J Determann… - Nature, 2012 - ideas.repec.org
Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal
current IDEAS home Advanced search Economic literature: papers, articles, software …

Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH Hellmer, F Kauker, R Timmermann, J Determann… - Nature, 2012 - go.gale.com
The Antarctic ice sheet loses mass at its fringes bordering the Southern Ocean. At this
boundary, warm circumpolar water can override the continental slope front, reaching the …

Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH Hellmer, F Kauker, R Timmermann, J Determann… - Nature, 2012 - epic.awi.de
The Antarctic ice sheet loses mass at its fringes bordering the Southern Ocean. At this
boundary, warm circumpolar water can override the continental slope front, reaching the …

Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current.

HH Hellmer, F Kauker, R Timmermann, J Determann… - Nature, 2012 - europepmc.org
The Antarctic ice sheet loses mass at its fringes bordering the Southern Ocean. At this
boundary, warm circumpolar water can override the continental slope front, reaching the …

Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH Hellmer, F Kauker, R Timmermann, J Determann… - Nature, 2012 - econpapers.repec.org
EconPapers: Twenty-first-century warming of a large Antarctic ice-shelf cavity by a
redirected coastal current EconPapers Economics at your fingertips EconPapers Home …
[PDF] core.ac.uk

[PDF][PDF] 21st-century warming of a large Antarctic ice shelf cavity by

HH Hellmer, F Kauker, R Timmermann, J Determann… - core.ac.uk
The Antarctic ice sheet loses mass at its fringes bordering the Southern 12 Ocean marginal
seas. At this boundary, warm circumpolar water can 13 override the continental slope front …

Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current

HH Hellmer, F Kauker, R Timmermann… - …, 2012 - pubmed.ncbi.nlm.nih.gov
The Antarctic ice sheet loses mass at its fringes bordering the Southern Ocean. At this
boundary, warm circumpolar water can override the continental slope front, reaching the …