Junior Group Marine Carbon and Ecosystem Feedbacks in the Earth System, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
Hartmut H. Hellmer
Physical Oceanography of the Polar Seas, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
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3,100
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PDF: 533
XML: 181
Total: 3,100
Supplement: 179
BibTeX: 181
EndNote: 166
Views and downloads (calculated since 10 Oct 2022)
Cumulative views and downloads
(calculated since 10 Oct 2022)
Total article views: 2,379 (including HTML, PDF, and XML)
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1,890
332
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2,379
179
167
156
HTML: 1,890
PDF: 332
XML: 157
Total: 2,379
Supplement: 179
BibTeX: 167
EndNote: 156
Views and downloads (calculated since 07 Nov 2023)
Cumulative views and downloads
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Total article views: 721 (including HTML, PDF, and XML)
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496
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721
14
10
HTML: 496
PDF: 201
XML: 24
Total: 721
BibTeX: 14
EndNote: 10
Views and downloads (calculated since 10 Oct 2022)
Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 3,100 (including HTML, PDF, and XML)
Thereof 3,011 with geography defined
and 89 with unknown origin.
Total article views: 2,379 (including HTML, PDF, and XML)
Thereof 2,297 with geography defined
and 82 with unknown origin.
Total article views: 721 (including HTML, PDF, and XML)
Thereof 714 with geography defined
and 7 with unknown origin.
Recently, it was found that cold-to-warm changes in Antarctic shelf sea areas are possible and lead to higher ice shelf melt rates. In modelling experiments, we found that if the highest density in front of the ice shelf becomes lower than the density of the warmer water off-shelf at the deepest access to the shelf, the off-shelf water will flow onto the shelf. Our results also indicate that this change will offer some, although not much, resistance to reversal and constitutes a tipping point.
Recently, it was found that cold-to-warm changes in Antarctic shelf sea areas are possible and...