Control of North Atlantic Deep Water circulation by the Greenland-Scotland Ridge

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Paleoceanography | / 2卷 / 157期

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[1] Control of North Atlantic deep water circulation by the Greenland-Scotland ridge
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[2] Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
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[3] Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
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[4] Increasing exchanges at Greenland-Scotland Ridge and their links with the North Atlantic Oscillation and Arctic Sea Ice
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[5] Neogene overflow of Northern Component Water at the Greenland-Scotland Ridge
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[8] Production of dense overflow waters feeding the North Atlantic across the Greenland-Scotland Ridge .2. An inverse model
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[9] The sensitivity of the Greenland-Scotland Ridge overflow to forcing changes
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[10] Topological Constraints by the Greenland-Scotland Ridge on AMOC and Climate
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