Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Enhanced ocean-atmosphere carbon partitioning via the carbonate counter pump during the last deglacial.Southern Ocean deep convection as a driver of Antarctic warming events Antarctic density stratification and the strength of the circumpolar current during the Last Glacial Maximum

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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Carina B Lange

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Helge W Arz

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Jérôme Kaiser

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Marc Wengler

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Naomi Harada

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Oscar Baeza-Urrea

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Rolf Kilian

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P2860

An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka

IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP

Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciation.

The last glacial termination.

On the role of the Agulhas system in ocean circulation and climate.

The Southern Ocean in the Coupled Model Intercomparison Project phase 5.

Responses of ocean circulation and carbon cycle to changes in the position of the Southern Hemisphere westerlies at Last Glacial Maximum.

Carbon isotope records reveal precise timing of enhanced Southern Ocean upwelling during the last deglaciation.

Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2.

One-to-one coupling of glacial climate variability in Greenland and Antarctica.

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13496-13501

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scholarly article

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10.1073/PNAS.1509203112

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English

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Glacial reduction and millennial-scale variations in Drake Passage throughflow

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P2860

P2860

Glacial reduction and millennial-scale variations in Drake Passage throughflow

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